East Star Resources - Apmintas Licence Drilling Results, Kazakhstan
Released
Released
Announcement PDF
RNS Number : 6466P
East Star Resources PLC
13 February 2023
THIS ANNOUNCEMENT CONTAINS INSIDE INFORMATION FOR THE PURPOSES OF ARTICLE 7 OF REGULATION
2014/596/EU WHICH IS PART OF DOMESTIC UK LAW PURSUANT TO THE MARKET ABUSE (AMENDMENT) (EU EXIT)
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13 February 2023
East Star Resources Plc
("East Star" or the "Company")
Apmintas Licence Drilling Results, Kazakhstan
Greater than 10 km of strike potential with demonstrated broad mineralised
intervals and high-grade intersections
East Star Resources Plc (LSE:EST), the Kazakhstan-focused mineral explorer, is pleased to provide results from
diamond drilling on the Apmintas Licence of the Chu-Ili Orogenic Gold Belt in Kazakhstan. Results show
anomalous gold mineralisation in all three target areas with potential economic grades in the Eshkilitau II and
Southern Shabdar targets.
Highlights:
·
·
·
·
·
Anomalous gold confirmed across all targets
Potential economic grade in the Eshkilitau II and Southern Shabdar targets
Eshkilitau II shows potential for a mineralised system with a strike of >1 km along a fault zone
Untested >10 km of strike potential along the fault controlled Eshkilitau trend
Best gold intersections include:
· Southern Shabdar
o AP_061 - 3 m @ 1.43 g/t from 48.9m and 1 m @ 32.15 g/t from 94.5 m
o AP_062 - 4 m @ 1.57 g/t from 72 m
o AP_067 - 3 m @ 2.11 g/t from 186 m
· Eshkilitau II
o AP_071 - 31 m @ 1.0 g/t from 61 m (including 6 m @ 1.83 g/t from 72 m and 7 m @ 1.52 g/t from
85 m)
o AP_072 - 4 m @ 2.35 g/t from 59 m
o AP_073 - 31m @ 1.27 g/t from 24 m (including 1 m @ 14.01 g/t from 24 m and 5 m @ 2.46 g/t from
43 m)
· Detailed structural logging underway with analysis to determine next steps to progress exploration
Alex Walker, East Star CEO, commented:
"The results of the drilling demonstrate gold bearing systems in all three target areas. Eshkilitau II shows potential for an
extensive mineralised system with a strike of more than 1 km along a fault zone. High-grade intersections at Southern
Shabdar (32.15 g/t Au) and Eshkilitau (14.01 g/t Au) demonstrate the existence of high-grade zones within the mineralised
systems while gold occurrences mapped over 10 km of the Eshkilitau trend demonstrate the exploration upside within the
region.
The Company has commenced detailed structural logging over mineralised sections of oriented core to better understand
structural controls and timing of mineralisation. This will expand our knowledge of the mineralisation system for the
planning of subsequent exploration.''
agram Description automatically generated with
low confidence
Figure 1 Over 10km of potential strike along the Eshkilitau trend
Eshkilitau II
The Eshkilitau group of occurrences are testing a possible orogenic gold system, bound to the
Ergenektin fault zone, related to quartz veins in sedimentary rocks and form a northwest striking
trend with Altynsai gold deposit to the southeast. The total length of the trend is about 10 km
historically explored by 77 trenches and seven prospecting shafts, over three Eshkilitau group
occurrences. The gold grades in trench samples range from 0.1 (below detection limits) to 2.0 g/t
Au with two samples at Eshkilitau II returning 168.0 and 200.8 g/t Au. Gold grades from drilling
often reported above 2 g/t Au and some intersections demonstrated mineralised intervals greater
than 5 m (Figure 2). Future exploration aims to further confirm these results as only historical
reports document the results (no historical material was available to validate).
Diagram,
generated
map
Description
automatically
Figure 2: Eshkilitau II demonstrating potential economic grades over 1 km of strike
The Eshkilitau II target was drill tested with AP_071, AP_072 AP_073, AP_074, AP_075, and
AP_076, totalling 632.4 m to a maximum depth of 125.6 m. The drilling intersected very coarse
grained polymictic metaconglomerate with lesser medium to coarse grained sandstones. The
metasediments are weathered to a depth of ~50 m depth and are strongly altered by intervals of
alternating chlorite and hematite (Figure 3).
A picture containing diagram Description automatically generated
Figure 3: Alternating alteration and deformed lithology in AP_071
The entire metasedimentary package is cut by several generations of cross-cutting quartz veins
with altered selvages. The structural deformation of these lithologies is notably more complex
with generations of cross cutting veins, faults, joints, and a seemingly more ductile deformation
regime than the other target areas - Southern Shabdar and Novoe in the Apmintas licence. The
samples show that several intervals carry grade including:
· AP_071 - 31 m @ 1.0 g/t from 61 m (including 6 m @ 1.83 g/t from 72 m and 7 m @ 1.52 g/t from 85 m)
· AP_072 - 4 m @ 2.35 g/t from 59 m
· AP_073 - 31m @ 1.27 g/t from 24 m (including 1 m @ 14.01 g/t from 24 m and 5 m @ 2.46 g/t from 43 m)
Currently, East Star is undertaking an analysis of the genesis of the mineralisation, including the
lithological and structural controls on mineralisation. The outcomes of this analysis will determine
the next steps in the 2023 exploration programme.
Southern Shabdar
The Southern Shabdar target is based over a historical drill target. A total of 77 drill holes drilled
as fences to an average depth of 90 m with a maximum depth of 300.5 m were previously drilled.
The historical drill holes reported gold values of 1 - 38.6 g/t over 2 m sample intervals. In 2022,
Southern Shabdar was drill tested with AP_061, AP_062, AP_063, AP_064, AP_066, AP_067, and
AP_068, totalling 1,572.7 m.
The geology intersected is generally grey medium grained diorites, granodiorites, and lesser dark
grey andesites. The host rocks are weathered to a depth of ~ 70 m depth. The diorites and
andesites are generally unaltered except for intervals cut by veinlets and stockworks. Several
intervals of quartz veining are noted with chlorite-epidote-sericite alteration associated with the
veinlets as selvages in the narrowly constrained lamina. The diorites are frequently cut by a later
fine grained ultramafic intrusive that displaces the diorites with quartz veining.
2022 drilling demonstrated intervals carrying significant grade including:
· AP_061 returned 3 m @ 1.43 g/t from 48.9 m and 1 m @ 32.15 g/t from 94.5 m
· AP_062 returned 4 m @ 1.57 g/t from 71 m
· AP_067 returned 3 m @ 2.11 g/t from 182 m (including 1 m @ 5.17 g/t)
The alteration and mineralisation are similar to other structurally controlled gold deposits in the
region, and so structural analysis on the portions of the core that are orientated requires
evaluation against the local and regional structures, geophysics, and geochemistry to understand
if the area has potential for significant mineralisation.
Novoe
The Novoe target has several pits dug by artisanal workers targeting NE-SW striking veins and
veinlets dipping at ~70 SE. AP_052, AP_0521, AP_053, and AP_054 were drilled, totalling 882 m to
a maximum depth of 331 m.
The geology intersected is generally pale medium grained sandstones, weathered to a depth of
~50 m, intruded by a medium grained granodiorite. The sandstones are generally unaltered
except for intervals cut by veinlets and stockworks. Several small intervals of quartz veining are
noted. These portions tend to have chlorite-epidote-sericite alteration associated with the veinlets
in intervals up to 15 m in width.
Most of the core with veining was sent for assay by initial spectral analysis followed by fire assay
confirmation of high-grade gold results. The assay results show broad zones of low-grade
mineralisation but only a few small intervals that carry significant grades. These intervals are
associated with increased density of alteration, veinlets/veinlets in stockworks, and sulphide
minerals associated with veining.
AP_052 and AP_0521 targeted the veins mined by artisanal workers at depth. These veins were
seemingly intersected by the Company's RC drilling in 2021 where AP_08 intersected 19 m @
14.36 g/t Au. However, these near-surface veins were not intersected by AP_052 and AP_0521,
demonstrating significant variability within the vein system. AP_052 did intersect a small quartz
vein stockwork interval at ~70 - 74 m depth which did not return significant grade.
Given the apparent structural complexity of the Novoe target, the Company intends to undertake
structural analysis on the portions of the core that are orientated and evaluate against the local
and regional structures, geophysics, and geochemistry to understand if the area has potential for
significant mineralisation that has been previously missed.
Laboratory and Assay Methodology
The analyses were conducted at Tsentre Geoanalit in Karaganda, Central Kazakhstan. This
laboratory is accredited by the State Standard of the Republic of Kazakhstan. The accreditation
certificate was registered in the State Register of the State Certification System of the Republic of
Kazakhstan on June 14, 2005 (No. КZ 7100000.06.10.00373). The laboratory is not accredited by
the international ISO17025 standard. A number of flame atomic absorption spectrometers of
various generations are in operation (PerkinElmer AAnalyst200, PerkinElmer Aanalyst400 and
PerkinElmer PinAAcle 900F) linked to Winlab32 AA Flame - Manual Analysis Control software. The
Apmintas samples were dissolved in aqua regia and subject to initial spectrograph analysis
followed by analysis of gold using AAS (using one of several PerkinElmer PinAAcle 900F units).
Samples were prepared at the Tsentrgeolsmyemka facility near Karaganda. Sample preparation
comprises weighing of the sample, drying, crushing to -1 mm, splitting of 300 g of sample by cone
and quarter, and milling using one of several rod mills. A sieve is available to check the crushing
quality. Milling takes approximately 5 hours and the quality of milling is determined by tactile test.
Half of the milled sample is placed in a hand labelled paper envelope and dispatched to the
analytical facility and the other half is kept on-site. The reject material is kept for five years. Cores
are kept in a shed at a different site in Karaganda.
A QA/QC programme was used to evaluate the quality of the 2804 total assay results. In total 137
QA/QC samples (or ~5%) were inserted into the sample stream including - 45 CRMs, 46 duplicates
and 46 blanks. The QA/QC samples returned satisfactory results demonstrating that the data are
acceptable for early stage exploration. It should be noted that the assays are likely to be under
reporting gold concentrations as the aqua regia solution is unlikely to completely dissolve the gold
in the samples. This is supported by the generally slightly lower than expected gold
concentrations seen in the CRM analyses.
For further information visit the Company's website at www.eaststarplc.com, or contact:
East Star Resources Plc
Alex Walker, Chief Executive Officer
Tel: +44 (0)20 7390 0234 (via Vigo Consulting)
Peterhouse Capital Limited (Corporate Broker and Placing Agent)
Duncan Vasey / Lucy Williams
Tel: +44 (0) 20 7469 0930
Vigo Consulting (Investor Relations)
Ben Simons / Peter Jacob
Tel: +44 (0)20 7390 0234
About East Star Resources Plc
East Star Resources is focused on the discovery and development of gold, rare earth, and copper deposits in
Kazakhstan. With an initial nine licences covering 1,687 square kilometres in three mineral rich districts, East Star is
undertaking an intensive exploration programme, applying modern geophysics and out-of-the-box geological
concepts to discover minerals under cover and at depths not previously explored. The Company also intends to
further expand its licence portfolio in Kazakhstan. East Star's management are based permanently on the ground,
supported by local expertise, and joint ventures with the state mining company.
Follow us on social media:
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www.eaststarplc.com/newsalerts
The person who arranged for the release of this announcement was Alex Walker, CEO of the Company.
Competent Person's Statement
Scientific or technical information in this disclosure related to exploration was reviewed by Dr
Tremain Woods, a full-time employee of MSA Minerals Consulting Ltd. Dr Woods is a member in
good standing with the Geological Society of South Africa. He has sufficient experience that is
relevant to the commodity, style of mineralization or type of deposit under consideration and
activity which he is undertaking to qualify as a Competent Person under the JORC code (2012
Edition).
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