Apollo Minerals Limited: High Grade and Tungsten Results From Newly Obtained Historical Data at the

Apollo Minerals Limited: High Grade and Tungsten Results From Newly Obtained Historical Data at the Couflens Project

ID: 587496

(firmenpresse) - HIGH GRADE GOLD AND TUNGSTEN RESULTS FROM NEWLY OBTAINED HISTORICAL DATA AT THE COUFLENS PROJECT

Highlights:
- Significant technical archive obtained from the historical Salau tungsten mine in France from the Bureau de Recherches Géologiques et Minières (BRGM) who previously undertook exploration research at and around the mine.
- The archive includes previously unavailable reports on gold assay results from 1986 from historical channel sampling and drilling inside the Salau mine including:
o up to 1.9m at 16 g/t gold from channel sampling programs, and
o 8.5m at 3.4 g/t gold, including 1.9m (at) 8.4 g/t gold, from diamond drilling results within the mine area.
- The historical gold assay results confirm the presence of high-grade gold values within the mine and at depths of approximately 700m below surface.
- Modern exploration undertaken by Apollo Minerals has identified the presence of comparable high-grade gold at surface and within historical tailings disposal areas.
- The presence of gold is now confirmed at surface along multiple kilometres of strike and down to depths of 600m inside the Salau mine. This highlights the significant scale potential of the exploration opportunity at the Project.
- The archive also has information on more than 1,000 drill holes and channel samples and contains over 100 boxes of geological maps, sections, drill logs as well as assays for tungsten from drilling.
- The archive will be reviewed and incorporated into the Companys existing database and 3D models and represents an additional saving in cost and time by de-risking the upcoming exploration and study programs.
- A program of in-mine channel sampling will occur in order to confirm the veracity of the historical data and to test for extensions to known mineralisation.

Hugo Schumann, Executive Director, commented:

We are excited by the high gold grades that were reported historically, including 8.5m at 3.4 g/t gold from drilling and 1.9m at 16 g/t gold from channel samples. These grades, reported from inside the mine, are comparable to the high gold grades obtained at surface have been identified along many kilometres of strike length.





This valuable archive obtained from the former mine operators greatly enhances our geological understanding of the historical Salau mine and regional potential of the Couflens Project. The fact that we now have access to more than 1,000 drill holes and channel samples represents a huge saving in cost and time and significantly de-risks our exploration programs.

Our focus is to rapidly commence a program of in-mine channel sampling and drilling immediately after the soon-to-be completed health and safety risk assessments.

For further information contact:

Hugo Schumann--
Tel: +44 207 478 3900 -
Email: info(at)apollominerals.com.au

Robert Behets
Tel: +61 8 9322 6322 -

INTRODUCTION

Apollo Minerals (Apollo Minerals or Company) is pleased to announce that it has obtained access to technical archives from Société Minière dAnglade, (SMA), which have been stored at the Bureau de Recherches Géologiques et Minières (BRGM) who undertook exploration and work programs for the SMA in and around the historical operations of the Salau mine.

The mine was previously one of the worlds highest-grade tungsten mines and remains open at depth with significant undeveloped gold potential.

HISTORICAL GEOLOGICAL AND DRILLING DATA

Following the acquisition of the Couflens Project in March 2017, the Company obtained a historical database comprising detailed geological logs and assay data from 56 diamond drill holes for 5,565m of surface drilling, 603 underground (UG) diamond drill holes for 45,396m, 155 UG rotary air blast holes for 1,737m and 2,373 UG channel samples for 6,367m.

In addition, the historical archives included detailed geological mine level plans and cross sections incorporating geological mapping of UG development and mine stoping areas. All of this data has been converted to digital format and used to create a 3D model of the Salau mine.

SMA TECHNICAL ARCHIVES

The Company has now been granted access to a second set of archives, the SMA technical archives (SMA Archives), which include combined assay data from more than 1,000 diamond, reverse circulation and rotary air blast drill holes and channel samples from historical exploration campaigns. In addition, the archives, which comprise over 100 boxes, containing technical reports, geological maps, sections and detailed drill logs.

This new information is now being reviewed and will be incorporated into the Companys existing 3D models of the mine. This additional information will further increase Companys understanding of the geology, mining and processing of the Salau deposit, lead to additional cost and time savings and de-risk the upcoming exploration and study programs

GOLD AND TUNGSTEN RESULTS WITHIN SMA ARCHIVES

High-grade gold was not sampled for as part of the mine operating procedures, and as a result was never recovered in milling nor a resource model developed.

Limited sampling of material from the lower section of the Veronique ore zone indicated the presence of high-grade gold (Fonteilles et al, 1989) however, the locations and details of this work were not well known to the Company.

Significantly, the new archives include a report documenting the sampling and analysis undertaken by the BRGM in 1986 of diamond drilling and channel samples and which report gold assays as well as the more typical tungsten (WO3) assays completed during mining.

The report documents 117 assay results of select intervals from 13 diamond drill holes and 13 channel samples, comprising of 71 and 46 assays respectively, from within the massive sulphide ore contained within the Veronique ore shoot and fault zone at approximately 600m below surface (figure 1).

Of the 13 channel sample locations, 10 contain samples of >1 g/t including 5.8m (at) 11.0 g/t gold. Of the 13 holes analysed, three contain >1 g/t gold values including SN481 with 8.5m (at) 3.4 g/t gold. A summary of significant results from the historical report are listed in Tables 1 and 2, with the complete listing of available assays within Appendix 2.

The Company intends, as discussed further below, to check and validate these and other historic results from the mine as part of its ongoing work programs.

Table 1: Summary of significant gold and tungsten results within diamond drilling results
Hole ILithology Width Au WO3
D (m) (g/t) (%)

SN481 Massive 8.5 3.4 2.0
sulphides

SN480 Granodiori1.2 2.8 1.5
te
and pyrrh
otite

DB74 Quartz. py0.5 3.0 1.2
rrhotite
and arsen
opyrite
NB: results as historically reported do not contain from and to intervals and locations are referenced to the logged occurrence of sulphides within the drill hole.

Table 2: Summary of significant gold results within channel sampling results
LocatiLithologyWidth Au WO3
on (m) (g/t) (%)

1253 EMassive 1.5 2.4 2.2
sulphide
s

1230 EMassive 0.4 2.0 2.5
sulphide
s

1194 EMassive 4.1 4.3 3.5
sulphide
s

1194 WSkarn 7.7 0.9 7.2
and

pyrrhotit
e

1173 EMassive 5.8 11.0 2.8
sulphide
s

1165 EMassive 8.0 9.5 2.4
sulphide
s

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Figure 1: Location of drill holes with anomalous gold from new SMA archives.

REGIONAL GOLD POTENTIAL
Work undertaken in recent years has demonstrated that the gold contained in the Salau deposit has potentially been largely underestimated and that the nature of the gold mineralisation had previously not been fully understood.

The Company has previously reported the gold assay results from exploration rock chip sampling at surface, as well as from the sampling of the historic tailings disposal areas from the former mine.

Exploration work has confirmed numerous gold occurrences around the historical Salau mine located on the margins of the major granodiorite intrusion. These gold occurrences are associated with fault structures and tungsten skarn mineralisation and have results of up to 24.50 g/t gold (refer to ASX announcement dated 29 November 2017).

Further high-grade mineralisation has also been identified up to 33.0 g/t gold with 2.03% WO3 at the Aurenere Project located approximately 6km to the west of the Salau deposit (refer to ASX announcement dated 27 March 2018). Additionally, high grade gold mineralisation of up to 3.34 g/t gold has been identified between these two locations and which is not associated with tungsten (Figure 2) (refer to ASX announcement dated 29 November 2017).

Recent geological mapping to support the health and safety program has identified fault zones and structures as well as sulphide and quartz zones that have not been previously sampled or mined due to their low tungsten content and which have a strong similarity to the outcrops at surface that returned significant gold values.

The new SMA Archive improves the Companys understanding of the gold distribution within and around the mine. It also highlights the potential for new discoveries of tungsten-gold and gold only occurrences within a highly prospective corridor that extends for over 10km along strike between Salau and the Aurenere Project in Spain. Furthermore, the fact that gold is present at surface, and at depths of 600m indicates the potential for significant scale.
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.
Figures 2 & 3: High grade gold results surrounding the Salau tungsten mine and within the wider region.
WORK PROGRAMS FOR THE COUFLENS PROJECT

The main focus of the Company remains the potential reactivation of the historical Salau
tungsten mine which was one of the worlds highest grade tungsten mine and forms the central part of the Couflens Project in France. At the same time, high grade gold and tungsten targets within the broader region, including both France and Spain, will be advanced to the drill ready stage.

Salau Mine Area (Couflens Project in France):

- Complete mine health and safety programs required to reopen mine for exploration activities;
- Mapping and channel sampling of mineralisation exposed in previously developed mine areas to:
o Confirm the veracity of historic data and information; and to
o Test for previously unexploited mineralisation;
- Underground drilling to confirm known zones of mineralisation and test for extensions
- of these zones; and
- Estimation and reporting of a Mineral Resource in accordance with the JORC Code.

- Regional exploration (Couflens and Aurenere Projects):

- Further surface exploration programs to assess the identified tungsten and gold
- prospects and advance them to the drill ready stage;
- Generation of new targets within the broader project areas and extensions to already
- identified zones of mineralisation;
- Drill planning and permit applications; and
- Continuing to progress the formal grant of the Investigation Permit for the Aurenere
- Project.

Competent Person Statement
The information in this announcement that relates to Exploration Results is based on information compiled by Mr Andrew Boyd of Cairn Consulting Limited, a Competent Person who is a Member of the Australian Institute of Geoscientists. Mr Boyd is a holder of shares, options and performance rights in, and is a key consultant of, Apollo Minerals Limited. Mr Boyd has sufficient experience which 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. Mr Boyd consents to the inclusion in this report of the statements based on his information in the form and context in which it appears.

Forward Looking Statements

Statements regarding plans with respect to Apollo Minerals projects are forward-looking statements. There can be no assurance that the Companys plans for development of its projects will proceed as currently expected. These forward-looking statements are based on the Companys expectations and beliefs concerning future events. Forward looking statements are necessarily subject to risks, uncertainties and other factors, many of which are outside the control of the Company, which could cause actual results to differ materially from such statements. The Company makes no undertaking to subsequently update or revise the forward-looking statements made in this announcement, to reflect the circumstances or events after the date of that announcement.


References
1. Fonteilles M., Soler P., Demange M., & Derré C., 1989; The Scheelite Skarn Deposit of Salau (Ariège, French Pyrenees), Economic Geology, Vol 84, pp 1172 - 1209

Appendix A: JORC Code, 2012 Edition - Table 1

Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)

CriteriJORC Code explanation Commentary
a

SamplinNature and quality of 117 rock samples were
g sampling collected as samples from
techni ( drill cores
ques eg cut channels, random and
chips, or specific chipped as channel samples
specialised industry from the
standard measurement
tools appropriate to the Salau mine as part of a histori
minerals under cal gold exploration program
investigation, such as undertaken by the BRGM in
down 1986.

hole gamma sondes, or
handheld XRF instruments, Location of samples and
selection of core was based
etc). These examples on presence of sulphides
should not be taken as related
limiting the broad
meaning of to existing WO3 mineralisation.
sampling.

Include reference to Sample size from channel
measures taken to ensure sampling in developments was
sample approximately 1kg in weight.
Where mineralisation was
representivity and the observed in drill cores,
appropriate calibration samples were collected to
of any measurement tools geological boundaries.
or systems
used.
Rock sample locations in
developments were surveyed
using historical mine plans
drawn by mine
surveyors.

Aspects of the Rock samples were collected
determination of from developments, with
mineralisation that are sample sizes of approximately
Material to the Public 1kg.
Report. In cases where
industry standard work Rock samples were transported
has been done this would to the
be relatively simple
( Salsigne mine laboratory in
eg reverse circulation southern
drilling was used to France
obtain 1 m samples from where gold analysis by fire
which 3 kg was pulverised assay was
to produce a 30 g charge undertaken.
for fire assay). In
other cases more No record of the gold sample
explanation may be preparation
required, such as where
there is coarse gold that or sample sizes is provided in
has inherent sampling the historic
problems. Unusual reports.
commodities or
mineralisation types Tungsten was historically
( analysed by
eg submarine nodules) may
warrant disclosure of AA after a tri-acid leach durin
detailed g the life of the
information. mine.

DrillinDrill type (eg core, Drill holes were drilled by
g reverse circulation, SMA. Drill cores were BQ (27
techni open-hole hammer, rotary mm) in diameter. The cores
ques air blast, auger, Bangka, were not
sonic, oriented.

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).
Drill Method of recording and Not available from historic
sample assessing core and chip records
recove sample recoveries and .
ry results
assessed.


Measures taken to maximise Drilling details not available
sample recovery and from historic records.
ensure representative Sampling was undertaken to
nature of the geological
samples. boundaries.

Whether a relationship Not available from historic
exists between sample records.
recovery and grade and
whether sample bias may
have occurred due to
preferential loss/gain

of fine/coarse material.
LoggingWhether core and chip Lithology of rock samples was
samples have been described by SMA geologists
geologically and with details

geotechnically logged to a being entered by Company staff
level of detail to into an Excel based Geological
support appropriate Database
Mineral Resource for future use
estimation, mining
studies and metallurgical
studies.

Whether logging is Logging was qualitative support
qualitative or ed
quantitative in nature.
Core (or costean, by petrographical description
channel,

etc) photography.
The total length and All the drill cores were
percentage of the logged.
relevant intersections
logged.

Sub-samIf core, whether cut or ½ BQ core was analysed.
pling sawn and whether quarter,
techni half or all core
ques taken.

and If non-core, whether Chip samples were not further
sample riffled, tube sampled, sub-sampled.
prepar rotary split,
ation
etc and whether sampled
wet or
dry.

For all sample types, the Rock samples from historical
nature, quality and BRGM gold exploration program
appropriateness of the were transported to the
sample preparation
technique. Salsigne laboratory in
southern
France
where analysis was undertaken
by

fire assay.
Gold result quality is not
documented within the
historical reporting and was
orientation in
nature.

Quality control procedures Not available from historic
adopted for all records
sub-sampling stages to
maximise

representivity of samples.
Measures taken to ensure Sample size from channel
that the sampling is sampling in developments was
representative of the in approximately 1kg in weight.
situ material collected, Where mineralisation was
including for instance observed in drill cores,
results for field samples were collected
duplicate/second-half
sampling. to geological boundaries
No field duplicates were
collected for the
samples.

Whether sample sizes are The scheelite can be either
appropriate to the grain fine grained (< 50µm) or
size of the material coarse grained (> 200µm),
being depending of the ore type.
sampled. Considering this variation,
the selected sample

volume size is appropriate.
QualityThe nature, quality and Samples were analysed at the Sa
of appropriateness of the lsigne
assay assaying and laboratory laboratory (Salsigne, France)
data procedures used and by fire
and whether the technique is assay
labora considered partial or . Detailed methods and
tory total. samples sizes are not
tests recorded within the

historical report.
For geophysical tools, Not applicable
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.

Nature of quality control Not available from historic
procedures adopted records
(
eg standards, blanks,
duplicates, external
laboratory checks) and
whether acceptable levels
of accuracy
(
ie lack of bias) and
precision

have been established.
VerificThe verification of Cross checking of data entry
ation significant intersections of historic results and
of by either independent or calculated intervals was by
sampli alternative company Company
ng and personnel. staff.
assayi
ng

The use of twinned holes. No twinned holes were used
Documentation of primary Historic data is provided as a
data, data entry written
procedures, data
verification, data seven page report by BRGM
storage (physical and staff.
electronic)
protocols. Data is entered into
controlled Excel templates
for validation.


Discuss any adjustment to None recorded within historic
assay report
data. .

LocatioAccuracy and quality of Location of rock sample
n of surveys used to locate locations were historically
data drill holes (collar and captured by mine
points down-hole surveys), survey
trenches, mine workings teams and recorded onto mine
and other locations used plans.
in Mineral Resource
estimation.

Specification of the grid Sample locations were converted
system from mine plans by Company
used. staff
into the GIS database in the
RGF93-Lambert
93 system.
Quality and adequacy of Topographic control is based
topographic on control visits of
control. historical channel sampling
sites.

Data Data spacing for reporting Rock samples were collected
spacin of Exploration from different sites and not
g and Results. on a fixed grid pattern.
distri
bution

Whether the data spacing The data spacing is not conside
and distribution is red sufficient to assume
sufficient to establish geological and grade
the degree of geological continuity.
and grade continuity
appropriate for the
Mineral Resource and Ore
Reserve estimation
procedure(s) and
classifications
applied.

Whether sample compositing No compositing of samples in
has been the field was
applied. undertaken.

OrientaWhether the orientation of In the Salau mine area, the
tion sampling achieves mineralised zone strikes
of unbiased sampling of east-west and is steeply
data possible structures and dipping (70°N to vertical).
in the extent to which this
relati is known, considering the The orientation of drilling
on to deposit and channel sampling is
geolog type. generally perpendicular to
ical this trend.
struct
ure

If the relationship No relationship between the
between the drilling drilling orientation and the
orientation and the orientation of key
orientation of key mineralised structures could
mineralised structures is be considered to have
considered to have introduced a sampling
introduced a sampling bias.
bias, this should be
assessed and reported if
material.

Sample The measures taken to Not available from historic
securi ensure sample records
ty security. .

Audits The results of any audits There has been no external
or or reviews of sampling audit or formal review of the
review techniques and techniques used or data
s data. collected by historical BRGM
gold exploration
program.

It is planned that the Company
undertake a comprehensive
program of resampling of the
historic mine works to
demonstrate the appropriate
validity

of the historic databases.

Section 2: Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)

CriteriaJORC Code explanation Commentary
Mineral Type, reference The Couflens Project comprises
tenemen name/number, location the
t and and ownership including
land agreements or material Couflens exploration licence (p
tenure issues with third ermis
status parties such as joint exclusif de recherches -
ventures, partnerships, PER) which covers an area
overriding royalties, of
native title interests, 42km
historical sites, 2 centred on the historical Sal
wilderness or national au
park and environmental mine.
settings. Apollo Minerals Limited
(Apollo Minerals) is the
100% owner of the

Couflens PER via its wholly
owned French subsidiaries

Variscan Mines SAS, Mines du Sa
lat
SAS and Ariege Tungstene SAS.
The Couflens PER was applied
for, and granted to,

Variscan Mines SAS. The PER
has been granted for an
initial period of five (5)
years commencing 11 February
2017,


The Couflens PER is located
adjacent to the village of

Salau and is located within a N
atura
2000 area with site code
FR7312003 with the
classification date
18/05/2015
.
The security of the Tenure in the form of a PER (pe
tenure held at the time rmis
of reporting along with exclusif de recherches, a
any known impediments to French exploration licence)
obtaining a licence to has been granted and is
operate in the considered secure. In
area. accordance with the French
Mining Code, the PER may be
extended for two additional
periods of a maximum of 5
years
each.

There are no known impediments
to obtaining a licence to
operate in this
area
other than any special
provisions based on the
existence of the
aforementioned

Natura 2000 site.
A tripartite convention was
signed between the Company,
the Prefecture of

Ariège, and the French
Ministry of Finance in March
2017, which requires the
Company to complete a
regulated program of health
and safety risk assessments
to ensure safe working
conditions inside the
historical

Salau tungsten mine before
exploration programs can
formally
commence.

ExploratAcknowledgment and Previous regional exploration
ion appraisal of exploration on
done by other
by parties. Couflens PER (outside Salau min
other e area) was undertaken by BRGM
parties during 1960s to 1980s. Work
completed included geological
mapping, geophysical surveys,
geochemical surveys, rock
sampling and diamond
drilling.

Historical geophysical surveys
included an airborne
(helicopter) electromagnetic
survey and ground based
magnetic, resistivity and
gravity surveys. Geochemical
surveys included stream
sediment sampling.


A detailed assessment of the
historic data is in progress.
No significant issues with
the data have been detected
to-date.

Geology Deposit type, geological The tungsten skarn
setting and style of mineralisation of the
mineralisation.
Salau deposit is hosted within
Devonian marbles adjacent to
the La

Fourque granodiorite. The miner
alisation typically occurs as
a 70°N to sub-vertical
dipping lenses occurring
between surface and

700m depth, and remain open at
depth. The style of the
tungsten mineralization
includes veins and
disseminated mineralization
in a fault called Veronique
related to late brittle
deformation.

Scheelite is the tungsten ore.
Most of the mineralisation is
hosted within Veronique shear
zone and contact metamorphism
aureole in marbles. This
deposit can be considered as
a tungsten skarn cross-cut by
a later auriferous shear-zone
system.

Drill A summary of all Collar positions are provided
hole information material to in Appendix B, Table
Informa the understanding of the 2.
tion exploration results
including a tabulation
of the following
information for all
Material drill
holes:

o easting and northing of
the drill hole
collar

o elevation or RL
(Reduced Level -
elevation above sea
level in metres) of the
drill hole
collar

o dip and azimuth of the
hole

o down hole length and
interception
depth

o hole length.
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.

Data In reporting Exploration No high-grade cuts have been
aggrega Results, weighting applied to the rock sample
tion averaging techniques, data
methods maximum and/or minimum reported
grade truncations . Significant grades as
( reported have been done on a
eg cutting of high grade x width weighted
grades) and cut-off basis.
grades are usually
Material and should be
stated.

Where aggregate No aggregation has been
intercepts incorporate applied to the rock sample
short lengths of high data
grade results and longer reported
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.

The assumptions used for No metal equivalent values are
any reporting of metal used.
equivalent values should
be clearly
stated.

RelationThese relationships are The geometry of the
ship particularly important mineralization is
between in the reporting of perpendicular to the drill
mineral Exploration Results. If holes. Interceptions with the
isation the geometry of the ore
widths mineralisation with
and respect to the drill with high angles (60 - 70°).

intercephole angle is known, its
t nature should be
lengths reported.

If it is not known and Relationships between
only the down hole mineralization geometry and
lengths are reported, drill
there should be a clear
statement to this effect hole angle are known.
(
eg down hole length,
true width not
known).

DiagramsAppropriate maps and Appropriate diagrams,
sections (with scales) including geological plans
and tabulations of and a long section
intercepts should be (interpreted), are included
included for any in the main body of this
significant discovery release.
being reported These
should include, but not
be limited to a plan
view of drill hole
collar locations and
appropriate sectional
views.

BalancedWhere comprehensive All results are reported in
reporti reporting of all Appendix
ng Exploration Results is
not practicable, B of this release.
representative reporting
of both low and high
grades and/or widths
should be practiced to
avoid misleading
reporting of Exploration
Results.

Other Other exploration data, In mine geological mapping was
substan if meaningful and completed in the whole
tive material, should be underground exploration area.
explora reported including (but This work program identified
tion not limited to): several additional high-grade
data geological observations; mineralized targets for both
geophysical survey tungsten and gold.
results; geochemical
survey results; bulk Surface gold exploration
samples - size and results are discussed in the
method of treatment; main body of this
metallurgical test release.
results; bulk density,
groundwater,
geotechnical and rock
characteristics;
potential deleterious or
contaminating
substances.

Further The nature and scale of Further exploration work
work planned further work planned for the
(
eg tests for lateral Couflens PER includes ongoing
extensions or depth review of the historical
extensions or exploration datasets and
large-scale step-out systematic follow-up rock
drilling). sampling, geophysical surveys
and drill program over
identified prospects and
exploration
targets.

A systematic sampling program
within the historic mine will
also be completed to test the
validity of the historic
databases.


Diagrams clearly These are shown in the main
highlighting the areas body of this
of possible extensions, release.
including the main
geological
interpretations and
future drilling areas,
provided this
information is not
commercially
sensitive.

Appendix B

Table B.1: Summary of Historical BRGM Rockchip Samples

SamplSamplOrebodyLocatThickWO3 Au Ag Lithology
e e ion ness (%) (ppm)(ppm)
numb type (m)
er

13106drillChristiS3 0.40 4.71< 0.27 Granodiorite
hol ne and
e
pyrrhotite
13107drill-------S3 0.15 0.08< 0.2< 1 Granodiorite
hole ----- and

pyrrhotite
13108drill-------S3 0.27 3.58< 0.28 Granodiorite
hole ----- and

pyrrhotite
13109drill-------S3 0.18 0.11< 0.2< 1 Granodiorite
hole ----- and

pyrrhotite
13110drill-------S3 0.86 4.41< 0.28 Granodiorite
hole ----- and

pyrrhotite
13126drill-------DB91 0.54 10.8< 0.210 Granodiorite
hole ----- 3 and

pyrrhotite
13127drill-------DB91 0.16 0.80< 0.2< 1 Granodiorite
hole ----- and

pyrrhotite
13111drillVeroniqSN4810.52 3.87< 0.210 Massive
hole ue sulphides
down
1165
west

13112drill-------SN4810.18 1.60< 0.2< 1 Massive
hole ----- sulphides

13113drill-------SN4810.25 0.782.6 11 Massive
hole ----- sulphides

13114drill-------SN4810.43 11.110.6 9 Massive
hole ----- 5 sulphides

13115drill-------SN4810.25 1.746.0 5 Massive
hole ----- sulphides

13116drill-------SN4810.37 7.877.8 3 Massive
hole ----- sulphides

13117drill-------SN4810.20 2.802.6 5 Massive
hole ----- sulphides

13118drill-------SN4810.66 2.0210.0 9 Massive
hole ----- sulphides

13119drill-------SN4810.26 1.440.3 1 Massive
hole ----- sulphides

13120drill-------SN4810.71 1.643.4 16 Massive
hole ----- sulphides

13121drill-------SN4810.90 0.29< 0.22 Massive
hole ----- sulphides

13122drill-------SN4813.03 0.732.2 6 Massive
hole ----- sulphides

13123drill-------SN4810.35 4.602.2 4 Massive
hole ----- sulphides

13124drill-------SN4811.11 1.242.2 10 Massive
hole ----- sulphides

13100drill-------SN4800.11 0.643.1 22 Granodiorite
hole ----- and

pyrrhotite
13101drill-------SN4801.10 1.632.8 5 Pyrrhotite an
hole ----- d

granodiorite
13102drill-------SN4800.12 0.35< 0.28 Granodiorite
hol ----- and
e
quartz
13103drill-------SN4800.11 2.85< 0.22 Granodiorite
hole ----- and

pyrrhotite
13104drill-------SN4800.18 0.17< 0.22 Granodiorite
hole ----- and
quartz

13105drill-------SN4800.55 1.00< 0.26 Granodiorite
hole ----- and

pyrrhotite
13090drill-------SN4790.33 5.20< 0.27 Quartz and py
hole ----- rrhotite

13091drill-------SN4790.27 1.16< 0.28 Skarn and pyr
hole ----- rhotite

13094drill-------SN4791.48 0.32< 0.29 Skarn and pyr
hole ----- rhotite

13095drill-------SN4790.34 0.99< 0.29 Skarn and pyr
hole ----- rhotite

13070drill-------SN4770.85 4.04< 0.21 Skarn and pyr
hole ----- rhotite

13077drill-------SN4770.37 6.27< 0.29 Skarn and pyr
hole ----- rhotite

13078drill-------SN4770.35 1.10< 0.27 Skarn and pyr
hole ----- rhotite

13079drill-------SN4771.04 1.200.2 10 Skarn
hole -----

13082drill-------SN4771.52 2.31< 0.2< 1 Pyrrhotite an
hole ----- d

granodiorite
13063drill-------SN4760.57 1.42< 0.22 Skarn and pyr
hole ----- rhotite

13067drill-------SN4760.63 2.22< 0.25 Skarn and pyr
hole ----- rhotite

13069drill-------SN4760.34 8.850.6 7 Skarn and pyr
hole ----- rhotite

13025drill-------DB81 2.32 2.39< 0.27 Skarn and pyr
hole ----- rhotite

13032drillVeroniqSN4720.20 3.02< 0.215 Massive
hole ue top sulphides
1165
west

13033drill-------SN4720.74 8.07< 0.26 Massive
hole ----- sulphides

13034drill-------SN4720.55 4.84< 0.25 Massive
hole ----- sulphides

12657drillVeroniqDB66 0.82 0.80< 0.28 Marble and py
hole ue rrhotite
down
1165
east

12658drill-------DB66 0.55 0.07< 0.27 Quartz
hole -----

12659drill-------DB66 0.66 0.55< 0.27 Marble and py
hole ----- rrhotite

12660drill-------DB66 0.34 0.15< 0.28 Marble and py
hole ----- rrhotite

12662drill-------DB66 1.30 4.650.2 9 Massive
hole ----- sulphides

12663drill-------DB66 0.30 1.55< 0.26 Massive
hole ----- sulphides

12664drill-------DB66 0.80 2.62< 0.25 Massive
hole ----- sulphides

12666drill-------DB66 0.75 4.88< 0.27 Skarn and pyr
hole ----- rhotite

12670drill-------DB66 0.76 3.96< 0.27 Massive
hole ----- sulphides

12671drill-------DB66 0.61 2.65< 0.2< 1 Massive
hole ----- sulphides

12673drill-------DB66 0.59 5.110.2 10 Skarn and pyr
hole ----- rhotite

12932drill-------DB76 0.16 1.520.2 11 Pyrrhotite an
hole ----- d
quartz

12935drill-------DB76 0.38 3.18< 0.28 Massive
hole ----- sulphides

12936drill-------DB76 0.79 9.58< 0.23 Massive
hole ----- sulphides

12938drill-------DB76 0.20 4.180.2 5 Massive
hole ----- sulphides

12939drill-------DB76 0.88 1.10< 0.2< 1 Massive
hole ----- sulphides

12940drill-------DB76 0.66 10.6< 0.2< 1 Massive
hole ----- 6 sulphides

12941drill-------DB76 0.65 4.020.3 10 Pyrrhotite an
hole ----- d
quartz

12827drill-------DB74 0.45 6.360.3 5 Massive
hole ----- sulphides
and

arsenopyrite
12828drill-------DB74 0.17 7.36< 0.24 Granodiorite
hole ----- and

pyrrhotite
12829drill-------DB74 0.18 0.50< 0.2< 1 Granodiorite
hole ----- and

pyrrhotite
12830drill-------DB74 0.32 13.00.4 6 Granodiorite
hole ----- 8 and

pyrrhotite
12831drill-------DB74 0.21 1.47< 0.27 Quartz and py
hole ----- rrhotite

12832drill-------DB74 0.58 4.39< 0.21 Quartz and py
hole ----- rrhotite

12833drill-------DB74 0.18 1.01< 0.25 Quartz and py
hole ----- rrhotite

12834drill-------DB74 0.68 4.83< 0.24 Quartz and py
hole ----- rrhotite

12835drill-------DB74 0.48 1.173.0 1 Quartz. pyrrh
hole ----- otite
and arsenopy
rite

13015drillVeroniqSN4710.29 1.261.5 1 Skarn and pyr
hole ue rhotite
1230
west

CS Chip VeroniqR19 1.70 6.190.4 6 Pyrrhotite an
7436Samp ue 1230 d
. west skarn

PA Chip -------1312 1.50 0.72< 0.23 Skarn and pyr
7510Samp ----- W rhotite
.
CS Chip Veroniq1281 0.40 4.533.6 9 Massive
7476Samp ue E sulphides
. east

PA Chip -------1281 1.10 2.900.4 5 Massive
7479Samp ----- E sulphides
.
PA Chip -------1281 2.00 1.550.4 9 Pyrrhotite an
7484Samp ----- E d
.
granodiorite
PA Chip -------1281 1.50 1.970.2 5 Granodiorite
7496Samp ----- E and
.
pyrrhotite
PA Chip -------1253 0.50 1.630.3 4 Massive
7505Samp ----- E sulphides
.
PA Chip -------1253 0.50 2.111.6 2 Massive
7511Samp ----- E sulphides
.
PA Chip -------1253 1.00 2.272.8 1 Pyrrhotite an
7504Samp ----- E d
. quartz

DM Chip -------1230 0.40 2.452.0 4 Massive
7257Samp ----- E sulphides
.
PA Chip -------1230 2.00 4.230.4 2 Pyrrhotite an
7243Samp ----- E d
. marble

DM Chip -------1230 1.40 2.901.6 2 Massive
7239Samp ----- E sulphides
.
PA Chip -------1230 2.00 2.211.9 2 Pyrrhotite.
7235Samp ----- E marble and
.
granodiorite
PA Chip Veroniq1230 1.40 5.550.4 6 Pyrrhotite an
7312Samp ue W d
. west
granodiorite
DM Chip -------1230 1.50 2.71< 0.2< 1 Pyrrhotite an
7306Samp ----- W d
. skarn

DM Chip -------1230 0.20 6.48< 0.2< 1 Pyrrhotite an
7301Samp ----- W d
. skarn

PA Chip -------1230 0.40 1.70< 0.23 Massive
7296Samp ----- W sulphides
.
CS 77Chip Veroniq1200 2.00 2.484.4 4 Massive
11 Samp ue E sulphides
. east

CS 77Chip -------1200 3.40 1.961.6 4 Massive
14 Samp ----- E sulphides
.
CS. 7Chip -------1200 1.50 4.242.8 < 1 Massive
723 Samp ----- E sulphides
.
CS 77Chip -------1208 1.50 1.872.2 < 1 Massive
41 Samp ----- E sulphides
.
PA Chip -------1194 0.50 5.631.0 1 Massive
7675Samp ----- E sulphides
.
PA 76Chip -------1194 1.00 2.645.4 1 Massive
64 Samp ----- E sulphides
.
PA Chip -------1194 1.00 3.252.6 3 Massive
7659Samp ----- E sulphides
.
PA Chip -------1194 1.30 2.565.4 4 Massive
7654Samp ----- E sulphides
.
PA Chip -------1194 0.80 6.213.2 < 1 Massive
7643Samp ----- E sulphides
.
PA Chip Veroniq1194 1.00 11.21.2 5 Skarn and pyr
7680Samp ue W 5 rhotite
. west

PA Chip -------1194 1.00 4.941.0 8 Pyrrhotite.
7693Samp ----- W skarn and
. marble

CS. 7Chip -------1194 0.90 4.401.4 < 1 Massive
683 Samp ----- W sulphides
.
PA Chip -------1194 2.00 5.500.8 4 Pyrrhotite an
7682Samp ----- W d
.
granodiorite
CS. 7Chip -------1194 0.30 0.830.4 16 Skarn and pyr
684 Samp ----- W rhotite
.
CS. 7Chip -------1194 0.70 8.571.0 7 Skarn and pyr
681 Samp ----- W rhotite
.
PA Chip -------1194 1.80 10.00.6 7 Massive
7679Samp ----- W 9 sulphides
.
PA Chip Veroniq1173 1.00 3.3214.0 5 Massive
7426Samp ue E sulphides
. east

CS. 7Chip -------1173 1.00 2.7910.0 5 Massive
430 Samp ----- E sulphides
.
CS. 7Chip -------1173 0.90 2.729.0 9 Massive
468 Samp ----- E sulphides
.
CS. 7Chip -------1173 1.40 3.0012.0 8 Massive
483 Samp ----- E sulphides
.
PA Chip -------1173 1.50 2.4410.0 5 Pyrrhotite.
7485Samp ----- E marble and
.
arsenopyrite
CS. 7Chip -------1165 1.10 2.6914.0 11 Massive
364 Samp ----- E sulphides
.
CS. 7Chip -------1165 0.70 4.839.0 5 Massive
368 Samp ----- E sulphides
.
CS. 7Chip -------1165 1.90 2.0516.0 1 Granodiorite
370 Samp ----- E and
.
pyrrhotite
CS 73Chip -------1165 2.00 2.695.0 5 Pyrrhotite. g
77 Samp ----- E ranodiorite
. and marble
PA Chip -------1165 2.30 1.616.0 4 Granodiorite.
7379Samp ----- E marble and
.
pyrrhotite
CS. 7Chip Veroniq1165 2.00 2.600.8 5 Massive
467 Samp ue W sulphides
. west

CS. 7Chip -------1165 2.00 3.371.2 7 Marble. grano
471 Samp ----- W diorite
. and pyrrhoti
te

CS 74Chip -------1165 0.50 8.450.8 7 Massive
91 Samp ----- W sulphides
.


Table B.2: Location of reported drill holes.

Hole EastiNorthiRL LengtAzimutDip
ID ng ng (m) h h (o)
(m)
(o)
DB66 551816183611186147 210 -40
7 2

DB74 55176618360116746 204 -32
9 9

DB76 55176618360116792 204 -48
9 9

DB8

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Bereitgestellt von Benutzer: irw
Datum: 04.02.2019 - 08:02 Uhr
Sprache: Deutsch
News-ID 587496
Anzahl Zeichen: 66242

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"
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