52% INCREASE IN INDICATED CATEGORY OF MINERAL
RESOURCE
ANNOUNCEMENT TO THE TORONTO STOCK
EXCHANGE NOVEMBER 2015
SUBIACO, Western Australia, Nov.
5, 2015 /CNW/ - RTG Mining Inc. ("RTG", "the Company")
(TSX Code: RTG, ASX Code: RTG) is pleased to report
an update of the Mineral Resource for the Mabilo Project reported
in accordance with the JORC Code (2012) and National Instrument
43-101 – Standards of Disclosure for Mineral Projects. The
Indicated Mineral Resource category has significantly increased by
52% to 8.9Mt. The new Mineral Resource Statement (with significant
potential to grow with further drilling) delivers sufficient
resources to justify a Feasibility Study with a 10 year mine life,
which is expected to be finalised later in the current quarter.
The Indicated Mineral Resource includes significant high grade
oxide gold and copper at shallow levels which contains 67,100
ounces of gold, 32,100t of copper and 320,800t of iron.
There remains significant scope for further expansion of the
resource. The magnetite skarn mineralisation, which makes up the
significant portion of the Mineral Resource is well defined and
remains open, down plunge and along strike.
Highlights of the resource include: –
- Total Indicated Resource of 8.9Mt at 1.92% Cu, 2.03g/t Au,
9.79g/t Ag and 45.56 Fe, containing 169,800t copper and
577,600oz of gold at a 0.3g/t Au cut-off grade (Table1).
- Total Inferred Resource of 3.9Mt at 1.46% Cu, 1.47g/t Au,
9.09g/t Ag and 29.02% Fe, containing 57,000t copper and
184,900oz of gold at a 0.3g/t Au cut-off grade (Table 1).
- Indicated Oxide Resource that includes a high grade oxide
gold "cap" zone (385,000t @ 2.9g/t Au) and a very high grade
Supergene Chalcocite zone (102,000t @ 23.0% Cu) at
shallow levels (Table 2).
- Significant upside potential remains to upgrade the Inferred
Resource and to further extend the magnetite skarn mineralisation
along strike and down dip beyond the current resource model.
Mineral Resource
Estimate Results - Reporting at 0.3 g/t Au lower cut-off - Mabilo
South and North Deposits
|
Classification
|
Weathering
|
Million
Tonnes
|
Cu
%
|
Au
g/t
|
Ag
g/t
|
Fe
%
|
Contained
Au ('000s Oz)
|
Contained Cu
('000s t)
|
Contained Fe
('000s t)
|
Cu
Equivalent*
('000s t)
|
Indicated
|
Oxide +
Supergene
|
0.78
|
4.1
|
2.7
|
9.7
|
41.2
|
67.1
|
32.1
|
320.8
|
45.7
|
Indicated
|
Fresh
|
8.08
|
1.7
|
2.0
|
9.8
|
46.0
|
510.5
|
137.7
|
3,713.7
|
264.1
|
Indicated
|
Total All
Materials
|
8.86
|
1.9
|
2.0
|
9.8
|
45.6
|
577.6
|
169.8
|
4,034.5
|
309.8
|
Inferred
|
Oxide +
Supergene
|
0.05
|
7.8
|
2.3
|
9.6
|
26.0
|
3.5
|
3.7
|
12.3
|
4.2
|
Inferred
|
Fresh
|
3.86
|
1.4
|
1.5
|
9.1
|
29.1
|
181.5
|
53.3
|
1,121.8
|
96.3
|
Inferred
|
Total All
Materials
|
3.91
|
1.5
|
1.5
|
9.1
|
29.0
|
184.9
|
57.0
|
1,134.1
|
100.5
|
Note: The Mineral
Resource was estimated within constraining wireframe solids based
on the mineralised geological units. The Mineral Resource is quoted
from all classified blocks above a lower cut-off grade 0.3 g/t Au
within these wireframe solids. Differences may occur due to
rounding.
|
* Cu equivalent is
calculated using the following formula which incorporates recovery
factors from metallurgical test work:
Cu Equivalent = ((75.2%*Au Oz)*$1,200)+((92.8%*Cu
Tonnes)*$5,200)+((88.4%*Fe Tonnes)*$65)+((60%*Ag
Oz)*$16))/$5,200
|
Table 1 - Total Mabilo Resource at 0.3 g/t Au Cut-off
Grade
OXIDE STRATEGY
The Indicated Oxide Resource includes a high grade oxide gold
"cap" zone (385,000t @ 2.9g/t Au) and a very high grade Supergene
Chalcocite zone (102,000t @ 23.2% Cu) at shallow levels (Table
2). Given the high grade nature of this shallow oxide
mineralisation, this area will be the focus of the initial
development strategy. (See Figure 1).
Indicated
|
South Mineralised
Zone
|
Million
Tonnes
|
Au
g/t
|
Cu
%
|
Fe
%
|
Contained
Au
|
Contained
Cu
('000s
t)
|
Contained
Fe
|
('000s
oz)
|
('000s
t)
|
Oxide Gold
Cap
|
0.33
|
3.1
|
0.2
|
42.6
|
33.3
|
0.7
|
142.2
|
Oxide
Copper/Gold
|
0.28
|
2.4
|
2.6
|
44
|
21.6
|
7.1
|
121.4
|
Supergene
Chalcocite
|
0.1
|
2.3
|
23.2
|
38.4
|
7.6
|
23.7
|
39.2
|
Sub-Total
|
0.71
|
2.7
|
4.4
|
42.5
|
62.5
|
31.5
|
302.8
|
North Mineralised
Zone
|
|
|
|
|
|
|
|
Oxide Gold
Cap
|
0.05
|
1.9
|
0.2
|
29.7
|
3
|
0.1
|
15.1
|
Oxide
Copper/Gold
|
0.02
|
2.8
|
3
|
17.7
|
1.5
|
0.5
|
3
|
Sub
Total
|
0.07
|
2.1
|
0.9
|
26.7
|
4.6
|
0.6
|
18
|
Total
|
0.78
|
2.7
|
4.1
|
41.2
|
67.1
|
32.1
|
320.8
|
Inferred
|
North Mineralised
Zone
|
Million
Tonnes
|
Au
g/t
|
Cu
%
|
Fe
%
|
Contained
Au
|
Contained
Cu
('000s
t)
|
Contained
Fe
|
('000s
oz)
|
('000s
t)
|
Oxide Gold
Cap
|
0.02
|
1.7
|
0.2
|
27.6
|
1.2
|
0.1
|
6
|
Oxide
Copper/Gold
|
0.01
|
1.9
|
2.3
|
20.8
|
0.8
|
0.3
|
2.6
|
Supergene
Chalcocite
|
0.01
|
3.6
|
26
|
28.2
|
1.5
|
3.4
|
3.6
|
Sub
Total
|
0.05
|
2.3
|
7.8
|
26
|
3.5
|
3.7
|
12.3
|
|
Note: The Mineral
Resource was estimated within constraining wireframe solids based
on the mineralised geological units. The resource is quoted from
all classified blocks above a lower cut-off grade 0.3 g/t Au within
these wireframe solids. Differences may occur due to
rounding
|
Table 2 - Oxide Gold and Chalcocite Copper Mabilo Resource at
0.3g/t Au Cut-off Grade
PRIMARY STRATEGY
The majority of the Mabilo Project value is contained within the
primary resource representing 91% of the 8.86Mt defined Indicated
tonnes. Figure 2 highlights the magnetite skarn in the Southern
Mineralised Zone. This resource contains significant Indicated
tonnes of Copper-Gold-Iron Skarn. Initial resource work focused on
clearly defining the Oxide Resource. Drilling since the maiden
resource was announced has focused on better defining the
copper-gold-magnetite skarn to provide confidence in the Mineral
Resource for the Feasibility Study currently being finalised.
The majority of the Mabilo Project primary resource is the
magnetite skarn of the North and South Mineralised zones. The
magnetite skarn in the North Mineralised Zone is relatively higher
in grade at 2.43% Cu and 2.21g/t Au compared to that in the south
at 1.67% Cu and 2.01g/t Au. The shallow plunging and down dip
extending South Mineralised Zone contains the majority of the
tonnes and is a primary focus for the Company. The North
Mineralised Zone magnetite skarn resource occurs at shallower
levels and will be used to supplement the South Mineralised Zone
and contains significant true widths and higher tonnes.
RTG Chief Executive Officer, Justine
Magee said that this is the second mineral resource for the
Mabilo Project, and underpins the long term potential of the
project.
"The second Mineral Resource, delivered in less than 18
months from investing in the project, demonstrates a significant
opportunity for the Company, The mineralized zones remain open
along strike, down dip and down plunge with significant exploration
upside from other untested areas within the tenement." Ms
Magee said.
ABOUT MABILO
The Mabilo Project is located in Camarines Norte Province,
Eastern Luzon, Philippines (Figure
3). It comprises one granted Exploration Permit (EP-014-2013-V) of
approximately 498 ha (currently in renewal process) and two
Exploration Permit Applications (EXPA-000188-V) of 2,737 ha and
(EXPA 0000 209-V) of 498 ha. The Project area is relatively flat
and is easily accessed by 15 km of all-weather road from the
highway at the nearby town of Labo.
Summary of Mineral Resource Estimate and Reporting
Criteria
The Mineral Resource was prepared by independent resource
consultancy CSA Global Pty Ltd ("CSA Global").
Geology and Geological Interpretation
Two mineralised magnetite skarn bodies were initially targeted
using ground magnetic data and have been subsequently drilled. The
magnetite skarn mineralisation is parallel to the host carbonate
unit and passes down-dip into garnet skarn, contact metamorphosed
marble or limestone. Magnetite skarn represents the replacement
bodies of the limestone marble lithologies. Magnetite skarn bodies
have been fault off-set laterally with magnetite continuing across
offset zones as strongly mineralised magnetite breccias.
Magnetite near surface has been subject to tropical weathering
and the development of an oxide zone dominated by a significant
gold-rich, copper-depleted cap (referred to as Oxide Gold "Cap"). A
high grade chalcocite zone dominates the northern end of the South
Zone with the remainder of the oxide resource being oxidised
magnetite skarn with similar copper and gold grades to primary
magnetite.
The North Mineralised Zone and South Mineralised Zone have both
been modelled for this Mineral Resource Estimate ("MRE").
Mineralised skarn is dipping 60 degrees to the southwest and
striking approximately 320 degrees. The North Mineralised Zone is
approximately 160m in strike length and is fault offset 150m from
the larger South Mineralised Zone which is approximately 500m in
strike length. The South Mineralised Zone is fault offset into two
fault blocks. The thickness of magnetite skarn is variable due to
lithological variation of the host marble limestone. At the
southern end of the South Mineralised Zone, magnetite is
approximately 30m in thickness, thinning down dip to approximately
15m at the marble contacts (Figure 4). At the northern end of the
South Mineralised Zone the thickness is approximately 45-50m where
it has been subjected to oxidation and supergene enrichment before
being covered by volcanic lahars and tuffs. The North Mineralised
Zone is up to 60m thick, and thinning to 15m at the
magnetite-marble contact.
The skarn has been subjected to extensive retrograde alteration.
This includes variable overprint of the magnetite skarn by pyrite.
Drilling and Sampling Techniques
The MRE is based on data obtained from 98 diamond core drill
holes (18,200.90m) drilled across the two mineralised zones. Drill
holes are located on a nominal 40m by 40m spacing across primary
magnetite zones with good geological continuity. Oxide and
chalcocite zones were drilled at 25m by 20m nominal spacing with
drilling oriented approximately north-west to south-east across the
strike of mineralisation. The dip of the drill holes was designed
to intersect the mineralisation at the optimal angle to minimise
sampling bias with a number of early vertical holes followed up
with angled holes. All drill results included in the MRE have been
reported in previous releases.
The majority of the drill hole collars were surveyed using a
differential global positioning system ("DGPS") to centimetre
accuracy. All down-hole surveying was carried out using a
combination of Reflex Ez-Trak multi-shot survey tool at 30m
intervals down hole and the Reflex Gyro system was used where
magnetite skarn was intersected.
All diamond drill core was geologically logged, recording
relevant data to a set template. Diamond core was also
geotechnically logged and the core photographed for future record.
Diamond core was half core sampled to geology contacts. Core
samples were submitted for analysis to ISO-certified Intertek
McPhar Laboratory in Manila. Field
quality assurance procedures were employed, including the use of
standards, blanks and duplicates. The drill hole data is maintained
in a secure relational database by company personnel.
Sample Analysis Method
Half core samples were cut and sent for analysis to Intertek
McPhar Laboratory, an independent ISO-certified laboratory in
Manila. Samples were crushed and
pulverised (95% <75 ɥm). Gold was analysed by 50g Fire Assay and
the other elements including copper and iron by ICP-MS (Inductively
Coupled Plasma Mass Spectrometry) or ICP-OES (Inductively Coupled
Plasma Optical Emission Spectrometry) following a four-acid
digest.
The sample preparation and assay techniques used for the assay
results reported herein are of international industry standard and
can be considered total. As a result, Iron grade though dominated
by Iron in magnetite, includes Iron in other minerals including
chalcopyrite and pyrite.
Resource Estimation Methodology
Datamine Studio 3 software was used for all geological
modelling, block modelling, grade interpolation, Mineral Resource
classification and reporting. Mineralisation domains were modelled
based on the geological interpretation from the lithological
logging of drill core and drill sample assay results. For the
magnetite skarn zones, which are by definition mineralised with
magnetite iron, the lithological logging has driven the
interpretation. Other lithological units in the system are not
necessarily mineralised to potentially economic levels throughout
their full extents. These zones have been modelled using a nominal
lower cut-off grade combination of 0.3g/t Au and 0.3% Cu in concert
with the lithological logging to generate mineralised lithological
domains.
The block model consists of 41 mineralisation lenses grouped
into 14 lithological domain zones of Cu-Au-Fe mineralisation, based
on lens lithology type. There are 9 mineralised lithological domain
zones in the South Mineralised Zone and 5 in the North Mineralised
Zone. The mineralised lithological domain zones were used as hard
boundaries to select sample populations for data analysis and grade
estimation. In the South Mineralised Zone hard boundaries between
individual lenses were used in the grade estimation, while soft
boundaries between the lenses within each domain zone were used in
the North Mineralised Zone (refer to Figure 5).
Sample data was composited to 1m downhole lengths based on
sample length frequency. Statistical analysis was undertaken on all
mineralised zones and high grade cuts were applied based on a
review of the histograms, probability plots and basic
statistics.
Grade interpolation was undertaken using ordinary kriging
("OK") with an inverse distance to the power of two ("IDS") check
estimate. Search ellipsoids were oriented to reflect
mineralisation continuity directions identified from sample data
analysis.
Block model definition parameters were reviewed with the primary
block size of 10m E-W by 10m N-S by 5m vertical and sub-blocking to
2.5m by 2.5m by 2.5m.
Note the iron grade in the MRE is total iron. Although dominated
by magnetite iron in the magnetite skarn, it does include other
iron-bearing minerals including pyrite which will not be
economically recoverable.
Cut-off Grades
Cut-off grades for reporting the Mineral Resource are 0.3g/t Au,
in line with recommendations from RTG based on preliminary
optimisation studies.
Classification Criteria
The Mineral Resource is classified as Indicated and Inferred, in
accordance with the JORC (2012) Code, with geological evidence
sufficient to assume geological and grade continuity in the
Indicated volumes. Classification of the Mineral Resource estimate
was carried out taking into account the geological understanding of
the deposit, quality of the samples, density of data and drill hole
spacing.
ABOUT RTG MINING INC
RTG Mining Inc. is a mining and exploration company listed on
the main board of the Toronto Stock Exchange and Australian
Securities Exchange Limited. RTG is focused on developing the
high grade copper/gold/magnetite Mabilo Project and advancing
exploration on the highly prospective Bunawan Project, both in
the Philippines, while also
identifying major new projects which will allow the Company to move
quickly and safely to production.
RTG has an experienced management team (previously responsible
for the development of the Masbate Gold Mine in the Philippines through CGA Mining Limited),
and has B2Gold as one of its major shareholders in the Company.
B2Gold is a member of both the S&P/TSX Global Gold and Global
Mining Indices.
CAUTIONARY NOTE REGARDING FORWARD LOOKING STATEMENTS
This announcement includes certain "forward-looking statements"
within the meaning of Canadian securities legislation. Statement
regarding interpretation of exploration results, plans for further
exploration and accuracy of mineral resource and mineral reserve
estimates and related assumptions and inherent operating risks, are
forward-looking statements. Forward-looking statements involve
various risks and uncertainties and are based on certain factors
and assumptions. There can be no assurance that such statements
will prove to be accurate, and actual results and future events
could differ materially from those anticipated in such statements.
Important factors that could cause actual results to differ
materially from RTG's expectations include uncertainties related to
fluctuations in gold and other commodity prices and currency
exchange rates; uncertainties relating to interpretation of drill
results and the geology, continuity and grade of mineral deposits;
uncertainty of estimates of capital and operating costs, recovery
rates, production estimates and estimated economic return; the need
for cooperation of government agencies in the development of RTG's
mineral projects; the need to obtain additional financing to
develop RTG's mineral projects; the possibility of delay in
development programs or in construction projects and uncertainty of
meeting anticipated program milestones for RTG's mineral projects
and other risks and uncertainties disclosed under the heading "Risk
Factors" in RTG's Annual Information Form for the year ended
31 December 2014 filed with the
Canadian securities regulatory authorities on the SEDAR website at
sedar.com.
QUALIFIED PERSON AND COMPETENT PERSON STATEMENT
The information in this release that relates to exploration
results at the Mabilo Project is based upon information prepared by
or under the supervision of Robert Ayres
BSc (Hons), who is a Qualified Person and a Competent
Person. Mr Ayres is a member of the Australian Institute of
Geoscientists and a full-time employee of Mt Labo Exploration and
Development Company, a Philippine mining company, an associate
company of RTG Mining Limited. Mr Ayres has sufficient experience
that is relevant to the style of mineralisation and type of deposit
under consideration and to the activity being undertaken, to
qualify as a Competent Person as defined in the 2012 Edition of the
"Australasian Code for Reporting of Exploration Results, Mineral
Resources and Ore Reserves" and to qualify as a "Qualified Person"
under National Instrument 43-101 – Standards of Disclosure for
Mineral Projects ("NI 43-101"). Mr. Ayres has verified the data
disclosed in this release, including sampling, analytical and test
data underlying the information contained in the release. Mr. Ayres
consents to the inclusion in the release of the matters based on
his information in the form and the context in which it
appears.
The information in this release that relates to Mineral
Resources is based on information prepared by or under the
supervision of Mr Aaron Green, who
is a Qualified Person and Competent Person. Mr Green is a Member of
the Australian Institute of Geoscientists and is employed by CSA
Global Pty Ltd, an independent consulting company. Mr Green has
sufficient experience that is relevant to the style of
mineralisation and type of deposit under consideration and to the
activity which he is undertaking to qualify as a Competent Person
as defined in the 2012 Edition of the "Australasian Code for
Reporting of Exploration Results, Mineral Resources and Ore
Reserves" and to qualify as a "Qualified Person" under National
Instrument 43-101 – Standards of Disclosure for Mineral Projects
("NI 43-101"). Mr. Green has verified the data disclosed in this
release, including sampling, analytical and test data underlying
the information contained in the release. Mr Green consents to the
inclusion in the release of the matters based on his information in
the form and context in which it appears.
Appendix 1: Location of Infill Drill Holes Previously Not
Reported
All drill holes included in the Mineral Resource Estimate have
been previously reported. All collars were surveyed using a
differential global positioning system ("DGPS") to centimetre
accuracy.
Appendix 2: JORC Code 2012 Edition Table
1
Section 1 Sampling Techniques and Data
|
|
|
Criteria
|
JORC Code
explanation
|
Commentary
|
Sampling
techniques
|
- Nature and quality of sampling (e.g. cut
channels, random chips, or specific specialised industry standard
measurement tools appropriate to the minerals under investigation,
such as down hole gamma sondes, or handheld XRF instruments, etc).
These examples should not be taken as limiting the broad meaning of
sampling.
|
- The assay data reported herein is based on
sampling of diamond drill core of PQ, HQ and NQ diameter which was
cut with a diamond core saw. Samples are generally of 1 m length,
although occasionally slightly longer or shorter where changes in
lithology, core size or core recovery required adjustments; samples
are not more than 2 m length.
|
- Include reference to measures taken to
ensure sample representivity and the appropriate calibration of any
measurement tools or systems used.
|
- The length of each drill run is
recorded and the recovery for each run calculated on site and
checked again at the core shed. Certified reference standards and
blank samples were submitted to assess the accuracy and precision
of the results and every 20th sample was sawn into two and the two
quarter core samples submitted for analysis separately as a
duplicate sample.
|
- Aspects of the determination of
mineralisation that are Material to the Public Report.
|
- Half core samples were cut and sent for
analysis by an independent ISO-certified laboratory (Intertek
McPhar Laboratory) in Manila. Samples were crushed and pulverised
(95% <75 μm). Gold was analysed by 50 g Fire Assay and the other
elements including copper and iron by ICP-MS (Inductively Coupled
Plasma Mass Spectrometry) or ICP-OES (Inductively Coupled Plasma
Optical Emission Spectrometry) following a four-acid digest.
|
Drilling
techniques
|
- Drill type (e.g. core, reverse
circulation, open-hole hammer, rotary air blast, auger, Bangka,
sonic, etc) and details (eg core diameter, triple or standard tube,
depth of diamond tails, face-sampling bit or other type, whether
core is oriented and if so, by what method, etc).
|
- Drilling was by PQ, HQ and NQ diameter,
triple tube diamond coring. The core was not orientated.
|
Drill sample
recovery
|
- Method of recording and assessing core and
chip sample recoveries and results assessed.
|
- Core recovery is initially measured on site
by trained technicians and by the supervising geologist. Any core
loss is measured, the percentage is calculated and both are
recorded in the geotechnical log for reference when assessing assay
results.
|
- Measures taken to maximise sample recovery
and ensure representative nature of the samples.
|
- All care is taken to ensure maximum recovery
of diamond core and drillers are informed of the importance of core
recovery. Any areas of poor core recovery are sampled separately
thus assay results can be directly related to core recovery. The
majority of the mineralisation is in fresh rock where recoveries
are greater than 90%. Most mineralisation occurs in wide
intersections of massive magnetite skarn with relatively uniform
copper and gold grades. Core loss occurs in fracture zones but is
usually not a significant problem i.e. the core lost in fracture
zones is unlikely to have been significantly higher or lower grade
than the surrounding material. In the weathered hematitic oxidised
zones some core loss is unavoidable, but overall recovery is
generally >90% and the core loss is volumetrically minor in the
mineralised zones. In areas of poor recovery, the sample intervals
are arranged to coincide with drill runs, thus areas of different
core loss percentage are specific to individual samples which can
be assessed when interpreting analytical results and modelled in
future resource estimation studies. Where an area of 100% core loss
is identified the sample intervals are marked to each side of the
zone and the zone is designated "No core" and assigned zero value
in the various log sheets and geochemical database.
|
- Whether a relationship exists between
sample recovery and grade and whether sample bias may have occurred
due to preferential loss/gain of fine/coarse material.
|
- There is no discernible relationship between
core recovery and grade. The skarn bodies are relatively uniform
over significant lengths and the copper and gold grades are not
related to clay and fracture zones which are the main causes of
core loss.
|
Logging
|
- Whether core and chip samples have been
geologically and geotechnically logged to a level of detail to
support appropriate Mineral Resource estimation, mining studies and
metallurgical studies.
|
- Diamond drill core for each entire drill hole
was logged in significant detail in a number of logging sheets
including a geological log, a structural log, a geotechnical log
and a magnetic susceptibility log for the entire drill hole.
Mineralised and sampled intervals are logged individually in a
separate quantitative mineral log with percentages of the different
copper minerals being recorded. The logging is appropriate for
Mineral Resource estimates and mining studies.
|
- Whether logging is qualitative or
quantitative in nature. Core (or costean, channel, etc.)
photography.
|
- Most of the geological logging is a mixture
of qualitative (descriptions of the various geological features)
and quantitative (numbers and angles of veins and fracture zones,
mineral percentages etc.). Both the mineralisation log and the
magnetic susceptibility log are quantitative. Photographs are taken
of all core (both wet and dry) prior to the core being
cut.
|
- The total length and percentage of the
relevant intersections logged.
|
- All core, including barren overburden is
logged in the various logging sheets noted above apart from the
quantitative mineralisation log in which only the mineralised
intervals sent for geochemical analysis are logged in greater
detail.
|
Sub-sampling
techniques and sample preparation
|
- If core, whether cut or sawn and whether
quarter, half or all core taken.
|
- All sampling data is from diamond drill core.
Samples are of sawn half core except for duplicate samples which
are quarter core. Half core is bagged and sent to an ISO-certified
independent laboratory for analysis. The other half retained for
reference and/or further testwork.
|
- If non-core, whether riffled, tube
sampled, rotary split, etc and whether sampled wet or dry.
|
- Not applicable for diamond core
drilling.
|
- For all sample types, the nature, quality
and appropriateness of the sample preparation technique.
|
- All core samples were dried, crushed to 95%
<10 mm and a 1.5 kg sub-sample is separated using a riffle
splitter and pulverised to 95% <75 μm. A 50 g sub-sample
is utilised as a Fire Assay charge for gold analysis. The
sample preparation technique and sub-sampling is appropriate for
the mineralisation.
|
- Quality control procedures adopted for all
sub-sampling stages to maximise representivity of samples.
|
- Blank samples and duplicate samples are
submitted routinely to monitor the sampling and analytical process
and to ensure that samples are representative of in situ material.
One in every 20 samples of half core is sawn again to produce two
quarter core duplicate samples which are submitted to the
laboratory separately with different sample numbers. A blank sample
was inserted into sample batches at every
20thsample.
|
- Measures taken to ensure that the sampling
is representative of the in situ material collected, including for
instance results for field duplicate/second-half sampling.
|
- The magnetite skarn mineralisation occurs in
extensive zones of magnetite skarn with disseminated chalcopyrite,
containing gold. The sample size of approximately 1 m core length
is suitable in respect to the grain size of the
mineralisation.
|
- Whether sample sizes are appropriate to
the grain size of the material being sampled.
|
- The sample size is considered appropriate for
the material sampled. It is believed that grain size has no bearing
on the grade of the sampled material.
|
Quality of
assay data and laboratory tests
|
- The nature, quality and appropriateness of
the assaying and laboratory procedures used and whether the
technique is considered partial or total.
|
- All core samples were analysed at an
ISO-certified independent laboratory. Gold was analysed by 50 g
Fire Assay and the other elements including copper and iron were
analysed by ICP-MS or ICP-OES following a four acid digest. The
sample preparation and assay techniques are of international
industry standard and can be considered total.
|
- For geophysical tools, spectrometers,
handheld XRF instruments, etc, the parameters used in determining
the analysis including instrument make and model, reading times,
calibrations factors applied and their derivation, etc.
|
- No geophysical tools were used for any
analysis reported herein. Magnetic susceptibility readings are used
in magnetic modelling but are not used to estimate magnetite or Fe
content.
|
- Nature of quality control procedures
adopted (e.g. standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy (ie lack of bias)
and precision have been established.
|
- Quality control completed by RTG included
analysis of standards, blanks, and duplicates. Commercial Certified
Reference Materials were inserted into sample batches every
40thsample. A blank sample was inserted every
20thsample; the blank sample material has been sourced
and prepared from a local quarry. One in every 20 core samples is
cut into 2 quarter core samples which were submitted independently
with their own sample numbers. In addition, Intertek conducted
their own extensive check sampling as part of their own internal
QA/QC processes which is reported in the assay sheets. A record of
results from all duplicates, blanks and standards is maintained for
ongoing QA/QC assessment. Examination of all the QC sample data
indicates satisfactory performance of field sampling protocols and
the assay laboratory.
|
Verification of
sampling and assaying
|
- The verification of significant
intersections by either independent or alternative company
personnel.
|
- Significant mineralisation intersections were
verified by alternative company personnel.
|
- The use of twinned holes.
|
- No twinned holes have been drilled.
|
- Documentation of primary data, data entry
procedures, data verification, data storage (physical and
electronic) protocols.
|
- Data documentation, verification and storage
is conducted in accordance with RTG's Standard Operating Procedures
Manual for the Mabilo Project. The diamond drill core is manually
logged in significant detail in a number of separate Excel template
logging sheets. Logging is recorded manually on logging sheets and
transcribed into protected Excel spreadsheet templates or entered
directly into the Excel templates. The data are validated by both
the Project Geologist and the company Database Manager and uploaded
to the dedicated project database where they are merged with assay
results reported digitally by the laboratory. Hard copies of all
logging sheets are kept at the Project office in Daet.
|
- Discuss any adjustment to assay
data.
|
- No adjustments have been made to assay
data.
|
Location of
data points
|
- Accuracy and quality of surveys used to
locate drill holes (collar and down-hole surveys), trenches, mine
workings and other locations used in Mineral Resource
estimation.
|
- Drill-hole collars are initially surveyed
with a hand-held GPS with an accuracy of approximately +/- 5 m.
Completed holes are surveyed by an independent qualified surveyor
on a periodic basis using standard differential GPS (DGPS)
equipment achieving sub-decimetre accuracy in horizontal and
vertical position.
|
- Specification of the grid system
used.
|
- Drill collars are surveyed in UTM WGS84 Zone
51N grid.
|
- Quality and adequacy of topographic
control.
|
- The Mabilo project area is relatively flat
with total variation in topography less than 15 m. Topographic
control is provided by DGPS surveying.
|
Data spacing
and distribution
|
- Data spacing for reporting of Exploration
Results.
|
- Drill holes are planned on a nominal grid
with 20 m between drill holes on 40 m spaced lines.
|
- Whether the data spacing and distribution
is sufficient to establish the degree of geological and grade
continuity appropriate for the Mineral Resource and Ore Reserve
estimation procedure(s) and classifications applied.
|
- The drill hole spacing was designed to
determine the continuity and extent of the mineralised skarn zones.
Based on statistical assessment of drill results to date, the
nominal 40 x 20 m drill hole spacing is sufficient to support
Mineral Resource estimation.
|
- Whether sample compositing has been
applied.
|
- No compositing of intervals in the field was
undertaken.
|
Orientation of
data in relation to geological structure
|
- Whether the
orientation of sampling achieves unbiased sampling of possible
structures and the extent to which this is known, considering the
deposit type.
|
- No bias
attributable to orientation of sampling upgrading of results has
been identified.
|
- If the
relationship between the drilling orientation and the orientation
of key mineralised structures is considered to have introduced a
sampling bias, this should be assessed and reported if
material.
|
- No bias
attributable to orientation of sampling upgrading of results has
been identified.
|
Sample
security
|
- The measures
taken to ensure sample security.
|
- Chain of custody is
managed by RTG employees. Samples were stored in secure storage
from the time of drilling, through gathering and splitting.
Remaining core is kept in a secure compound at the Company regional
office in Daet town and guarded at night. Samples are sent directly
from the core shed to the laboratory packed in secured and sealed
plastic drums using either Company vehicles or a local transport
company. A standard Chain of Custody form is signed by the driver
responsible for transporting the samples upon receipt of samples at
the core yard and is signed by an employee of the laboratory on
receipt of the samples at the laboratory. Completed forms are
returned to the Company for filing.
|
Audits or
reviews
|
- The results of
any audits or reviews of sampling techniques and
data.
|
- The sampling
techniques and QA/QC data are reviewed on an ongoing basis by
Company management and independent consultants.
|
Section 2 Reporting of Exploration Results
|
|
|
Criteria
|
JORC Code
explanation
|
Commentary
|
Mineral
tenement and land tenure status
|
- Type, reference
name/number, location and ownership including agreements or
material issues with third parties such as joint ventures,
partnerships, overriding royalties, native title interests,
historical sites, wilderness or national park and environmental
settings.
|
- The Mabilo Project
is covered by Exploration Permit EP-014-2013-V and Exploration
Permit Application EXPA-000188-V and EXPA 0000 209-V. EP-014-2013-V
was issued to Mt Labo Exploration and Development Corporation ("Mt
Labo"), an associated entity of RTG Mining Inc. There is a 1%
royalty payable on net mining revenue received by Mt Labo in
relation to EP-014-2013-V.
Mt Labo has entered into a
joint venture agreement with Galeo Equipment and Mining Company,
Inc. ("Galeo") to partner in exploring and developing the Mabilo
and Nalesbitan Projects. To date, Galeo has earned a 36% interest
in the Projects.
Sierra Mining Limited ("Sierra"), a wholly owned subsidiary of RTG,
has entered into a MOU with Galeo whereby Galeo can earn an
additional 6% interest in the joint venture by mining the initial
1.5 Mt of waste at Mabilo or Nalesbitan and other requirements. The
MOU is subject to a number of conditions precedent, including
Sierra shareholder approval.
|
- The security of
the tenure held at the time of reporting along with any known
impediments to obtaining a license to operate in the
area.
|
- The tenure over the
area currently being explored at Mabilo is a granted Exploration
Permit which is currently being renewed. All documents are in good
standing and the renewal process is ongoing. There is no native
title or Indigenous ancestral domains claims at Mabilo.
|
Exploration
done by other parties
|
- Acknowledgment
and appraisal of exploration by other parties.
|
- The only
significant previous exploration over the Mabilo project area was a
drilling program at another site within the tenement and a ground
magnetic survey. RTG (or its predecessor Sierra) has reported this
data in previous reports to the ASX and used the ground magnetic
survey as a basis for initial drill siting. Subsequently RTG
conducted its own ground magnetic survey with closer spaced survey
lines and reading intervals which supersedes the historical
program. There was no known previous exploration in the area of the
reported Mineral Resource.
|
Geology
|
- Deposit type,
geological setting and style of mineralisation.
|
- Mineralisation at
Mabilo can be defined as a magnetite-copper-gold skarn which
developed where the magnetite-copper-gold mineralisation replaced
calcareous horizons in the Eocene age Tumbaga Formation in the
contact zone of a Miocene diorite intrusion.
|
Drill hole
Information
|
- A summary of all
information material to the understanding of the exploration
results including a tabulation of the following information for all
Material drill holes:
- easting and
northing of the drill hole collar
- elevation or RL
(Reduced Level – elevation above sea level in metres) of the drill
hole collar
- dip and azimuth
of the hole
- down hole length
and interception depth
- hole
length.
|
- All relevant drill
hole information has been previously reported to the ASX. No
material changes have occurred to this information since it was
originally reported.
|
- If the exclusion
of this information is justified on the basis that the information
is not Material and this exclusion does not detract from the
understanding of the report, the Competent Person should clearly
explain why this is the case.
|
- All relevant data
has been reported.
|
Data
aggregation methods
|
- In reporting
Exploration Results, weighting averaging techniques, maximum and/or
minimum grade truncations (e.g. cutting of high grades) and cut-off
grades are usually Material and should be stated.
|
- Not reporting
exploration results.
|
- Where aggregate
intercepts incorporate short lengths of high grade results and
longer lengths of low grade results, the procedure used for such
aggregation should be stated and some typical examples of such
aggregations should be shown in detail.
|
- Not reporting
exploration results.
|
- The assumptions
used for any reporting of metal equivalent values should be clearly
stated.
|
- Based on
preliminary metallurgical testwork undertaken by previous owners,
including flotation and magnetic separation, the following
assumptions for gold equivalents are:
Gold Price
US$1200/oz Gold recovery – 75.2%
Copper Price US$5,200t
Copper recovery – 92.8%
Silver Price US$16/oz
Silver recovery – 60%
Iron Price
US$65/t
Iron recovery – 88.4%
The calculation for copper equivalent
values was based on the following formula:
Cu Equivalent = ((75.2%*Au
Oz)*$1,200)+((92.8%*Cu Tonnes)*$5,200)+((88.4%*Fe
Tonnes)*$65)+((60%*Ag
Oz)*$16))/$5,200
|
Relationship
between mineralisation widths and intercept
lengths
|
- These
relationships are particularly important in the reporting of
Exploration Results.
|
- The Mabilo drill
have been drilled both vertically and inclined. The orientation of
the mineralised bodies is based on interpretation of geology from
drill holes supported by magnetic modelling which indicates that
much of the mineralisation is dipping to the southwest.
|
- If the geometry
of the mineralisation with respect to the drill hole angle is
known, its nature should be reported.
|
- The interpreted
orientation of the mineralised bodies is based on magnetic
modelling and drill-hole data and is documented in the report. The
fact that the intersections are in a dipping body and therefore not
true widths has been reported.
|
- If it is not
known and only the down hole lengths are reported, there should be
a clear statement to this effect (eg 'down hole length, true width
not known').
|
- No intervals
reported can be assumed to be a true width of the
mineralisation.
|
Diagrams
|
- Appropriate maps
and sections (with scales) and tabulations of intercepts should be
included for any significant discovery being reported These should
include, but not be limited to a plan view of drill hole collar
locations and appropriate sectional views.
|
- Refer to figures
within the main body of this report.
|
Balanced
reporting
|
- Where
comprehensive reporting of all Exploration Results is not
practicable, representative reporting of both low and high grades
and/or widths should be practiced to avoid misleading reporting of
Exploration Results.
|
|
Other
substantive exploration data
|
- Other
exploration data, if meaningful and material, should be reported
including (but not limited to): geological observations;
geophysical survey results; geochemical survey results; bulk
samples – size and method of treatment; metallurgical test results;
bulk density, groundwater, geotechnical and rock characteristics;
potential deleterious or contaminating substances.
|
- All meaningful
exploration data concerning the Mabilo Project has been reported in
previous reports to the ASX.
|
Further
work
|
- The nature and
scale of planned further work (e.g. tests for lateral extensions or
depth extensions or large-scale step-out drilling).
|
- Drilling is ongoing
at the Mabilo Project which will systematically test magnetic
bodies and step-out targets along strike and between the North
Mineralised Zone and the South Mineralised Zone as well as down-dip
from these zones.
|
|
- Diagrams clearly
highlighting the areas of possible extensions, including the main
geological interpretations and future drilling areas, provided this
information is not commercially sensitive.
|
- Refer to figures within the main body of this
report.
|
Section 3 Estimation and Reporting of Mineral
Resources
|
|
|
Criteria
|
JORC Code
explanation
|
Commentary
|
Database
integrity
|
- Measures taken to ensure that data has not
been corrupted by, for example, transcription or keying errors,
between its initial collection and its use for Mineral Resource
estimation purposes.
|
- Data used in the Mineral Resource estimate is
sourced from a data base export. Relevant tables from the data base
are exported to MS Excel format and converted to csv format for
import into Datamine Studio 3 software.
|
- Data validation procedures used.
|
- Validation of the data import include checks
for overlapping intervals, missing survey data, missing assay data,
missing lithological data, and missing collars.
|
Site
visits
|
- Comment on any site visits undertaken by
the Competent Person and the outcome of those visits.
|
- A representative of the Competent Person
("CP") has visited the project on several occasions, most recently
in October 2015. Diamond drilling programs were underway at Mabilo
during a previous site visit. The CP's representative was able to
review drilling and sampling procedures, as well as examine the
mineralisation occurrence and associated geological features.
Sample storage facilities and the analytical laboratory in Manilla
have also been inspected. There were no negative outcomes from any
of the above inspections, and all samples and geological data were
deemed fit for use in the Mineral Resource estimate.
|
- If no site visits have been undertaken
indicate why this is the case.
|
|
Geological
interpretation
|
- Confidence in (or conversely, the
uncertainty of) the geological interpretation of the mineral
deposit.
|
- The geology and mineral distribution of the
system is reasonably complex, and is being constantly refined as
more drilling is undertaken. As such the CP has taken a
conservative approach to Mineral Resource classification.
|
- Nature of the data used and of any
assumptions made.
|
- Drill hole intercept logging, assay results
and structural interpretations from drill core, and the results of
geophysical modelling of magnetic anomalies have formed the basis
for the geological interpretation. For the South Mineralised Zone
("SMZ") strike and depth extents have been reasonably well
constrained through drilling, except for the south eastern end
where the deposit is still open along strike and at depth and
assumptions have been made on the depth and strike extent of the
mineralisation. In the North Mineralised Zone ("NMZ") the strike
and depth extents of the mineralisation are not fully constrained
by drilling and assumptions have been made on the depth and strike
extents of the mineralisation based on the available information
including the geophysical modelling and bounding structure
interpretations. Some drill collars had not yet been surveyed by
DGPS at the time of modelling. The collars had been surveyed by
hand held GPS with an estimated horizontal accuracy (based on
historical comparisons) of roughly 3m. The elevation of the collar
has been corrected to the topographic surface. Mineralisation
intercepts from these drill holes were found to correspond well
with previously interpreted mineralisation zone extents. Any
differences from the true position is not expected to have any
material impact on the volumes and grades of the interpreted
mineralisation zones.
|
- The effect, if any, of alternative
interpretations on Mineral Resource estimation.
|
|
- The use of geology in guiding and
controlling Mineral Resource estimation.
|
- Geology has been the primary influence in
controlling the Mineral Resource estimation. Wireframes have
been constructed for the various lithological zones based on style
of mineralisation, host rock and oxidation state as determined by
the core logging and assaying.
|
- The factors affecting continuity both of
grade and geology.
|
|
|
- Continuity of geology and structures can be
identified and traced between drillholes by visual, geophysical and
geochemical characteristics. Breccia zones interpreted to relate to
fault structures have been noted in the drill core and have been
modelled.
|
Dimensions
|
- The extent and variability of the Mineral
Resource expressed as length (along strike or otherwise), plan
width, and depth below surface to the upper and lower limits of the
Mineral Resource.
|
- The SMZ is interpreted as having a 500 m
strike length, is 20 to 50 m in true width, with vertical depth
extent up to 280 m from roughly 50 m below surface. The NMZ has a
strike extent of roughly 160 m, true width between 20 m and 50 m
and depth extent of 135 m from roughly 40 m below surface.
|
Estimation and
modelling techniques
|
- The nature and appropriateness of the
estimation technique(s) applied and key assumptions, including
treatment of extreme grade values, domaining, interpolation
parameters and maximum distance of extrapolation from data points.
If a computer assisted estimation method was chosen include a
description of computer software and parameters used.
|
- The mineralisation has been estimated using
ordinary kriging ("OK") as the primary estimation method with an
inverse distance to the power 2 ("IDS") check estimate in Datamine
Studio 3 software. 41 mineralised lodes have been interpreted and
are grouped into 14 mineralised lithological domain zones of
Cu-Au-Fe mineralisation, based on lens lithology type and grade.
There are 9 of these zones in the SMZ and 6 zones in the
NMZ.
|
- The availability of check estimates,
previous estimates and/or mine production records and whether the
Mineral Resource estimate takes appropriate account of such
data.
|
- The mineralised lithological domain zones and
the individual mineralised lodes within them were used as hard
boundaries to select sample populations for data analysis and grade
estimation. For the SMZ hard boundaries between each interpreted
mineralisation lode have been used in the grade estimation while in
the NMZ soft boundaries between the grouped lodes within the
mineralised lithological domain zones and hard boundaries between
mineralised lithological domain zones have been used in the grade
estimation. Statistical analysis was completed on each zone to
determine appropriate top-cuts to apply to outlier grades of Fe,
Au, Cu and Ag where required.
|
- The assumptions made regarding recovery of
by-products.
|
- OK and IDS estimates are completed
concurrently in a number of estimation runs with varying
parameters. The results are compared against each other and the
drill hole results to ensure a reasonable estimate, that best
honours the drill sample data is reported. Comparison with the
previously reported estimate shows a roughly 12% increase in
tonnage and with a slight decrease in the mean reported grades
increases of between 3% and 10% of contained metal as detailed in
the relevant section of the Mineral Resource estimate
report.
|
- Estimation of deleterious elements or
other non-grade variables of economic significance (eg sulphur for
acid mine drainage characterisation).
|
- No mining has yet taken place at these
deposits.
|
- In the case of block model interpolation,
the block size in relation to the average sample spacing and the
search employed.
|
- Ag has been estimated and is assumed to be
also recoverable as part of the Au recovery processes. Fe grade
estimated in the MRE is total Fe. Although dominated by magnetite
Fe in the magnetite skarn, it does include other Fe-bearing
minerals including pyrite which will not be economically
recoverable.
|
- Any assumptions behind modelling of
selective mining units.
|
- Potentially deleterious As and S have been
estimated into the model to assist with future metallurgical work
and mining studies, but are not reported at this stage.
|
- Any assumptions about correlation between
variables.
|
- Interpreted domains are built into a
sub-celled block model with 10m E-W by 10m N-S by 5m vertical
parent block size. Parent block size is chosen based on being
roughly half the average drill spacing over the majority of the
deposit areas. Search ellipsoids for each estimation zone have been
orientated based on their geometry and grade continuity. Sample
numbers per block estimate and ellipsoid axial search ranges have
been tailored to geometry and data density of each zone to ensure
the majority of the model is estimated within the first search
pass. The search ellipse is doubled for a second search pass and
increased 20 fold for a third search pass to ensure all blocks were
estimated. Sample numbers required per block estimate have been
reduced with each search pass.
|
- Description of how the geological
interpretation was used to control the resource estimates.
|
- No assumptions have been made. Model minimum
sub-cell size is down to 2.5m N-S by 2.5m E-W by 2.5m
vertical.
|
- Discussion of basis for using or not using
grade cutting or capping.
|
- No assumptions have been made with each
element separately estimated. Statistical analysis shows a
generally good correlation between Au and Cu grades in unweathered
zones and poor correlation in weathered zones.
|
- The process of validation, the checking
process used, the comparison of model data to drill hole data, and
use of reconciliation data if available.
|
- Hard boundaries between each individual lode
have been used in the grade estimate for the SMZ. Soft boundaries
between the grouped lodes within the mineralised lithological
domain zones and hard boundaries between mineralised lithological
domain zones have been used in the grade estimation for the
NMZ.
|
|
- Statistical analysis to check grade
population distributions using histograms, probability plots and
summary statistics and the co-efficient of variation, was completed
on each zone for the estimated elements. Outlier grades were
variously found for most elements in the different mineralised
lithological domain zones and appropriate high grade cuts where
applied to remove undue influence of these outlier grades on the
grade estimation for each zone.
|
|
- Validation checks included statistical
comparison between drill sample grades, the OK and IDS estimate
results for each zone. Visual validation of grade trends for each
element along the drill sections was completed and trend plots
comparing drill sample grades and model grades for northings,
eastings and elevation were completed. These checks show reasonable
correlation between estimated block grades and drill sample grades.
No reconciliation data is available as no mining has taken
place.
|
Moisture
|
- Whether the tonnages are estimated on a
dry basis or with natural moisture, and the method of determination
of the moisture content.
|
- Tonnages have been estimated on a dry in situ
basis. No moisture values were reviewed.
|
Cut-off
parameters
|
- The basis of the adopted cut-off grade(s)
or quality parameters applied.
|
- For some lithological units nominal lower
cut-off grades of 0.3 g/t Au or 0.3 % Cu in concert with the
lithological logging were used to define continuous mineralised
lenses, in line with recommendations from RTG based on preliminary
optimisation studies.
|
Mining factors
or assumptions
|
- Assumptions made regarding possible mining
methods, minimum mining dimensions and internal (or, if applicable,
external) mining dilution. It is always necessary as part of the
process of determining reasonable prospects for eventual economic
extraction to consider potential mining methods, but the
assumptions made regarding mining methods and parameters when
estimating Mineral Resources may not always be rigorous. Where this
is the case, this should be reported with an explanation of the
basis of the mining assumptions made.
|
- It has been assumed that these deposits will
be amenable to open cut mining methods, and are economic to exploit
with this methodology at the reported average model grades. No
assumptions regarding minimum mining widths and dilution have been
made to date.
|
Metallurgical
factors or assumptions
|
- The basis for assumptions or predictions
regarding metallurgical amenability. It is always necessary as part
of the process of determining reasonable prospects for eventual
economic extraction to consider potential metallurgical methods,
but the assumptions regarding metallurgical treatment processes and
parameters made when reporting Mineral Resources may not always be
rigorous. Where this is the case, this should be reported with an
explanation of the basis of the metallurgical assumptions
made.
|
- The oxide portions of similar deposits in the
region are being successfully exploited by other entities, and it
is assumed that these zones can be economically exploited at the
modelled grades. For the unweathered or fresh materials ongoing
metallurgical testing has shown a less consistent response of the
samples tested than was expected. The initial findings indicate
there appears to be a relationship with S:Cu ratios involved in
metallurgical response. Composite samples appear to respond better
to flotation than the individual components that make up the
composites. Further optimisation testing is ongoing to improve
recoveries. Based on the results reported to date it is assumed
that a significant majority of the modelled unweathered
mineralisation can be economically exploited and will be readily
upgraded where necessary, using standard gravity, magnetic
processes and/or froth flotation concentration techniques as
appropriate for the different product streams.
|
Environmental
factors or assumptions
|
- Assumptions made regarding possible waste
and process residue disposal options. It is always necessary as
part of the process of determining reasonable prospects for
eventual economic extraction to consider the potential
environmental impacts of the mining and processing operation. While
at this stage the determination of potential environmental impacts,
particularly for a greenfields project, may not always be well
advanced, the status of early consideration of these potential
environmental impacts should be reported. Where these aspects have
not been considered this should be reported with an explanation of
the environmental assumptions made.
|
- No assumptions regarding possible waste and
process residue disposal options have been made. It is assumed that
such disposal will not present a significant hurdle to exploitation
of the deposit and that any disposal and potential environmental
impacts would be correctly managed as required under the regulatory
permitting conditions.
|
Bulk
density
|
- Whether assumed or determined. If assumed,
the basis for the assumptions. If determined, the method used,
whether wet or dry, the frequency of the measurements, the nature,
size and representativeness of the samples.
- The bulk density for bulk material must
have been measured by methods that adequately account for void
spaces (vugs, porosity, etc), moisture and differences between rock
and alteration zones within the deposit.
|
- In-situ dry bulk density values have been
applied to the modelled mineralisation based on linear regression
formulas for weathered and unweathered material separately. This is
based on reasonable correlations having been found between measured
bulk density results and Fe. Of the 1,009 measurements taken, 628
have assay result data, with 216 samples falling within the
interpreted mineralised zones. 29 samples fall within the oxide
mineralisation and density measurement shows a 73% correlation with
Fe grade. 188 measured density samples fall within the fresh
mineralisation with an 80% correlation between measured density and
Fe grade.
|
- Discuss assumptions for bulk density
estimates used in the evaluation process of the different
materials.
|
- Density measurements have been taken on drill
samples using wax coated water displacement methods, from all
different lithological types. CSA Global has noted the amount of
wax used in the coating process was excessive for some samples.
Analysis showed this issue generally only affects the oxide waste
and overburden zones. This means that waste density assigned to the
model could be over stated for the overburden and oxide zones.
There is a possibility that void spaces have been partially filled
by wax in the mineralisation zones affected by porosity, resulting
in a slightly higher density being calculated and assigned to some
zones. Any possible effects of this are expected to be within the
margins of error reflected by the classification.
|
|
- With the reasonable correlation between Fe
grade and bulk density, it is assumed that use of the regression
formulas describing this relationship is an appropriate method of
representing the expected variability in bulk density for the grade
estimated mineralised blocks. Analysis of the results of
application of the regression formulas to the model by individual
mineralised lithological domain unit shows that the mean model
density compares closely to the mean of the density measurements
from within each zone.
|
Classification
|
- The basis for the classification of the
Mineral Resources into varying confidence categories.
|
- Classification of the Mineral Resource
estimates was carried out taking into account the level of
geological understanding of the deposit, quality of samples,
density data and drill hole spacing.
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- Whether appropriate account has been taken
of all relevant factors (ie relative confidence in tonnage/grade
estimations, reliability of input data, confidence in continuity of
geology and metal values, quality, quantity and distribution of the
data).
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- The classification reflects areas of lower
and higher geological confidence in mineralised lithological domain
continuity based the intersecting drill sample data numbers,
spacing and orientation. Overall mineralisation trends are
reasonably consistent within the various lithotypes over numerous
drill sections.
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- Whether the result appropriately reflects
the Competent Person's view of the deposit.
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- The Mineral Resource estimate appropriately
reflects the view of the Competent Person.
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Audits or
reviews
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- The results of any audits or reviews of
Mineral Resource estimates.
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- Internal audits were completed by CSA Global
which verified the technical inputs, methodology, parameters and
results of the estimate.
No external audits have been undertaken.
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Discussion of
relative accuracy/ confidence
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- Where appropriate a statement of the
relative accuracy and confidence level in the Mineral Resource
estimate using an approach or procedure deemed appropriate by the
Competent Person. For example, the application of statistical or
geostatistical procedures to quantify the relative accuracy of the
resource within stated confidence limits, or, if such an approach
is not deemed appropriate, a qualitative discussion of the factors
that could affect the relative accuracy and confidence of the
estimate.
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- The relative accuracy of the Mineral Resource
estimate is reflected in the reporting of the Mineral Resource as
per the guidelines of the 2012 JORC Code.
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- The statement should specify whether it
relates to global or local estimates, and, if local, state the
relevant tonnages, which should be relevant to technical and
economic evaluation. Documentation should include assumptions made
and the procedures used.
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- The Mineral Resource statement relates to
global estimates of in-situ tonnes and grade.
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- These statements of relative accuracy and
confidence of the estimate should be compared with production data,
where available.
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- The deposit has not, and is not currently
being mined.
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SOURCE RTG Mining Inc.