28 August 2024
AIM: AAU
HIZARLIYAYLA DRILLING AND
GEOPHYSICS RESULTS
Potential for mineralisation
akin to the world-class Hod Maden deposit, 8.5km
south
Ariana Resources plc ("Ariana" or
"the Company") is pleased to announce a further set of results from
the Hizarliyayla area of the Salinbas Project and an outline of the
results of the geochemical study and geophysical survey over the
area. Ariana is an AIM-listed mineral exploration and development
company with gold project interests in Africa and Europe and owns
23.5% of Zenit Madencilik San. ve Tic. A.S. ("Zenit") in
partnership with Proccea Construction Co. (23.5%) and Ozaltin
Holding A.S. (53%). Hizarliyayla is 100% owned by
Zenit.
Highlights:
·
Final laboratory assay results received for the
Hizarliyayla drilling programme and reviewed in the context of new
geophysical and geochemical data.
·
Best intercepts to date include:
o HZR010 0.5m @ 3.96g/t Au + 28.65g/t Ag from 540.5m
o HZR009 0.7m @ 1.16% Cu + 0.72% Pb + 29.39g/t Ag from
293.3m
o HZR009 1.15m @ 0.76g/t Au + 22.09g/t Ag + 1.46% Zn from
300.0m
o HZR009 0.45m @ 1.59g/t Au + 47.28g/t Ag from 644.8m
o HZR010 0.4m @ 10% Zn + 2.38% Pb + 317.01g/t Ag from
662.3m
·
Geochemical and alteration zoning, particularly in
the vicinity of a north-south-trending subvertical structure, may
indicate proximity to a potentially mineralised porphyry intrusion
in a structural setting akin to the world-class Hod Maden deposit,
representing one of the highest margin development assets
globally.
·
Induced Polarisation survey for 12 line kilometres
completed, data processed and new targets defined, including a
significant set of coherent chargeability and resistivity anomalies
on the western flank of Hizarliyayla.
·
Additional c. 3,000m of diamond drilling
commencing for the Salinbas and Ardala areas to complete and partly
extend the original programme.
To
read a pdf version of the announcement, please click here: http://www.rns-pdf.londonstockexchange.com/rns/8662B_1-2024-8-27.pdf
Dr.
Kerim Sener, Managing Director, commented:
"The latest diamond drilling and geophysics results from the
Hizarliyayla exploration programme continue to demonstrate the
lateral extent and depth of the mineralised system. As we had
predicted from the geological model, most of the better intercepts
are located at deeper levels, in several places, below 500m from
the surface. This was always an ambitious and challenging
exploration programme. Still, these results have shown genuine
potential in this location for mineralisation akin to the nearby
and world-class Hod Maden deposit, located 8.5km south. The
opportunity at Hizarliyayla is therefore upgraded from a simple
test of the geological model to a demonstration of targets.
"In particular, an important new target has been identified on
the western flank of Hizarliyayla, which coincides with a porphyry
intrusion. The distribution of gold, copper, and molybdenum and the
alteration zonation in the periphery of this intrusion suggest that
the system is most well-developed in the northwest. Coincident
chargeability and resistivity anomalies in this area extend to the
surface and also correlate with the surface alteration. These
results support the interpretation that a mineralised porphyry
intrusion exists near Hizarliyayla, underscoring the importance of
further exploration in this area. Further work will be
undertaken to enhance the model to accommodate the latest results
and define targets within this system further. The
geophysical data, in particular, will be used to guide future
work.
"We are also pleased to announce the start-up of further
drilling at the Salinbas-Ardala area to complete and partly extend
the original drilling programme. This coincides with an
extensive re-examination of the geology and mineralisation, and we
are encouraged by the latest findings, which have further
strengthened our understanding of the prospectivity of the region
around the Ardala porphyry."
The
information contained within this announcement is deemed by the
Company to constitute inside information as stipulated under the
Market Abuse Regulations (EU) No. 596/2014 as it forms part of UK
Domestic Law by virtue of the European Union (Withdrawal) Act 2018
("UK MAR").
Drilling Programme
The Hizarliyayla prospect is located
9 kilometres southwest of the Salinbas and Ardala project area
towards the world-class Hod Maden Au-Cu deposit, about 8.5km
further south (Figure 1).
Hizarliyayla is defined by an area of approximately 1,500 metres by
800 metres, containing an argillic to advanced-argillic alteration
zone with pervasive disseminated pyrite, silica, and minor gold at
the surface.
Drilling commenced on the project in
late December 2022, and 10 drill holes have now been completed for
a total of 6,005.8 metres. The objective of the Hizarliyayla drilling programme
was to systematically test several soil geochemical targets and
intense clay alteration zones defined by prospect-scale mapping and
sampling.
Figure 1: Summary map showing
the completed drill hole collar positions for the Hizarliyayla
prospect. The inset topographic map shows the position of
Hizarliyayla with respect to Salinbas and Hod Maden, and the mining
licences comprising the Salinbas Project (red outline). The
location of the five IP/Resistivity survey lines are shown as
dotted black lines.
Drill holes were initially planned
to 200-300 metre depths; however, most holes intercepted far more
alteration and mineralisation than expected and so were continued
to a maximum depth range of 400-800 metres, with the deepest hole
being HZR010, which was drilled to 797 metres. All holes
intercepted sporadic intermediate sulphidation (Ag-Pb-Zn±Au) type
breccia and vein mineralisation, typically encountered in the
periphery of porphyry-style mineralisation (Figure 2). This was discussed in more
detail in an announcement of the Hizarliyayla discovery drilling
on
AIM: 21 June 2023.
Figure 2: Scaled map and
schematic long-section through the Hod Maden, Hizarliyayla and
Ardala/Salinbas areas, identifying the regular spacing of
hydrothermal (porphyry derived?) centres. The potentially most
well-preserved porphyry system within the project area occurs at
Hizarliyayla, and future drilling will need to be planned
accordingly.
The Hizarliyayla drilling programme
was completed in September 2023; with assay and multi-element
analysis recently completed at the Kiziltepe Mine Laboratory
("KML"). In total, 5,565 results (including 1,405 QA/QC samples)
for 6,737 metres of diamond core have been received from the KML;
previous results were announced on 6 December 2023 (Table 1, 2 and 3). Higher-grade intercepts (Table 1 and 2) are surrounded by sporadic halos of
lower-grade, but very extensive alteration and mineralisation
(Table 3).
All results for the Hizarliyayla
drilling programme have now been received.
Table 1: Significant gold and
silver intercepts calculated from the latest Hizarliyayla results,
using a 0.5g/t Au minimum cut-off and allowing for up to 1m
internal dilution. Copper, lead, and zinc values are shown for the
same intervals. Numbers in bold are considered significant for this
project.
Hole ID
|
From
(m)
|
To
(m)
|
Length
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
Cu
(%)
|
Pb
(%)
|
Zn
(%)
|
HZR007
|
198.9
|
199.3
|
0.4
|
0.55
|
1.74
|
0.02
|
0.02
|
0.09
|
HZR008
|
251.6
|
252.3
|
0.7
|
0.51
|
1.69
|
0.17
|
0.02
|
0.03
|
HZR009
|
293.3
|
294.0
|
0.7
|
0.78
|
29.39
|
1.16
|
0.72
|
0.33
|
300.0
|
301.2
|
1.15
|
0.76
|
22.09
|
0.44
|
0.54
|
1.46
|
644.8
|
645.2
|
0.45
|
1.59
|
47.28
|
0.01
|
0.26
|
0.75
|
HZR010
|
540.5
|
541.0
|
0.5
|
3.96
|
28.65
|
0.01
|
0.18
|
0.72
|
Table 2: Significant copper,
lead and zinc intercepts calculated from the latest Hizarliyayla
results, using a 0.1% Cu and 1% Pb and 1% Zn minimum cut-off. Gold
and silver values are shown for the same intervals. Numbers in bold
are considered significant for this project.
Hole ID
|
From
(m)
|
To
(m)
|
Length
(m)
|
Cu
(%)
|
Pb
(%)
|
Zn
(%)
|
Au
(g/t)
|
Ag
(g/t)
|
HZR007
|
188.0
|
189.0
|
1.0
|
0.14
|
0.02
|
0.04
|
0.24
|
2.56
|
286.1
|
286.4
|
0.3
|
0.02
|
0.39
|
1.52
|
0.09
|
5.60
|
414.3
|
414.7
|
0.4
|
0.04
|
1.82
|
1.02
|
0.13
|
135.75
|
HZR008
|
251.6
|
252.3
|
0.7
|
0.17
|
0.02
|
0.03
|
0.51
|
1.69
|
HZR009
|
291.0
|
292.3
|
1.3
|
0.25
|
0.25
|
0.61
|
0.15
|
7.49
|
293.3
|
294.0
|
0.7
|
1.16
|
0.72
|
0.33
|
0.78
|
29.39
|
300.0
|
301.2
|
1.1
|
0.44
|
0.54
|
1.46
|
0.76
|
22.09
|
HZR010
|
223.0
|
223.5
|
0.5
|
0.17
|
0.03
|
0.07
|
0.20
|
8.92
|
309.3
|
310.3
|
1.0
|
0.04
|
0.36
|
1.72
|
0.17
|
24.99
|
358.0
|
358.5
|
0.5
|
0.13
|
1.19
|
2.90
|
0.21
|
28.85
|
500.1
|
501.1
|
1.0
|
0.31
|
1.42
|
7.03
|
0.38
|
68.69
|
624.4
|
624.8
|
0.4
|
0.19
|
1.69
|
7.39
|
0.32
|
198.94
|
652.2
|
653.1
|
0.9
|
0.02
|
0.25
|
1.23
|
0.05
|
15.03
|
662.3
|
662.7
|
0.4
|
0.19
|
2.38
|
10.00
|
0.32
|
317.01
|
662.7
|
663.5
|
0.8
|
0.09
|
0.96
|
3.54
|
0.23
|
77.13
|
663.5
|
664.2
|
0.7
|
0.03
|
0.19
|
1.31
|
0.06
|
7.02
|
737.2
|
737.6
|
0.4
|
0.40
|
0.07
|
0.13
|
0.03
|
5.68
|
Table 3: Longer, lower-grade
gold and silver intercepts calculated from the latest Hizarliyayla
results using a 0.1g/t Au minimum cut-off.
Hole ID
|
From (m)
|
To (m)
|
Length (m)
|
Au (g/t
|
Ag (g/t)
|
HZR008
|
44.1
|
45.1
|
1.00
|
0.11
|
0.63
|
84.4
|
85.7
|
1.30
|
0.13
|
3.78
|
251.6
|
252.3
|
0.70
|
0.51
|
1.69
|
259.0
|
260.0
|
1.00
|
0.11
|
0.25
|
261.0
|
262.0
|
1.00
|
0.11
|
0.25
|
281.6
|
282.3
|
0.70
|
0.19
|
1.68
|
418.7
|
422.0
|
3.30
|
0.11
|
0.25
|
442.6
|
443.9
|
1.30
|
0.20
|
0.50
|
455.0
|
456.0
|
1.00
|
0.11
|
2.21
|
520.2
|
521.2
|
1.00
|
0.15
|
0.25
|
525.2
|
526.2
|
1.00
|
0.10
|
0.25
|
536.4
|
537.7
|
1.30
|
0.20
|
0.51
|
549.7
|
551.0
|
1.30
|
0.18
|
0.25
|
558.0
|
559.3
|
1.25
|
0.16
|
1.94
|
566.6
|
567.6
|
1.00
|
0.15
|
1.25
|
572.0
|
572.8
|
0.80
|
0.10
|
0.25
|
577.6
|
578.1
|
0.50
|
0.15
|
0.25
|
596.9
|
598.2
|
1.30
|
0.12
|
4.05
|
602.0
|
603.0
|
1.00
|
0.11
|
1.63
|
604.0
|
606.0
|
2.00
|
0.15
|
1.02
|
607.3
|
608.6
|
1.30
|
0.13
|
1.13
|
616.8
|
617.7
|
0.90
|
0.16
|
0.25
|
625.6
|
626.8
|
1.20
|
0.13
|
2.01
|
HZR009
|
162.6
|
163.6
|
1.00
|
0.13
|
1.12
|
191.2
|
191.8
|
0.60
|
0.13
|
0.76
|
192.4
|
193.7
|
1.30
|
0.13
|
0.53
|
261.7
|
264.0
|
2.30
|
0.12
|
0.25
|
277.0
|
278.0
|
1.00
|
0.12
|
0.25
|
291.0
|
292.3
|
1.30
|
0.15
|
7.49
|
293.3
|
294.0
|
0.70
|
0.78
|
29.39
|
300.0
|
301.2
|
1.15
|
0.76
|
22.09
|
304.7
|
305.7
|
1.00
|
0.10
|
1.64
|
306.5
|
307.8
|
1.30
|
0.11
|
1.49
|
339.7
|
340.0
|
0.30
|
0.45
|
1.18
|
438.5
|
439.7
|
1.20
|
0.13
|
0.25
|
445.1
|
445.6
|
0.50
|
0.45
|
0.25
|
547.6
|
550.6
|
3.00
|
0.38
|
3.87
|
568.3
|
569.1
|
0.80
|
0.12
|
0.25
|
644.8
|
645.2
|
0.45
|
1.59
|
47.28
|
HZR010
|
174.7
|
175.4
|
0.65
|
0.25
|
5.26
|
200.0
|
201.3
|
1.30
|
0.13
|
0.58
|
203.9
|
205.0
|
1.10
|
0.10
|
0.25
|
205.5
|
206.8
|
1.30
|
0.11
|
0.25
|
215.0
|
216.0
|
1.00
|
0.20
|
0.74
|
218.0
|
219.0
|
1.00
|
0.18
|
0.25
|
223.0
|
223.5
|
0.50
|
0.20
|
8.92
|
280.8
|
281.6
|
0.80
|
0.16
|
0.25
|
297.5
|
298.3
|
0.80
|
0.12
|
0.25
|
305.2
|
306.7
|
1.50
|
0.11
|
6.89
|
309.3
|
310.3
|
1.00
|
0.17
|
24.99
|
358.0
|
358.5
|
0.50
|
0.21
|
28.85
|
500.1
|
511.7
|
11.60
|
0.10
|
7.14
|
533.3
|
534.3
|
1.00
|
0.18
|
4.25
|
540.5
|
541.0
|
0.50
|
3.96
|
28.65
|
624.4
|
624.8
|
0.40
|
0.32
|
198.94
|
662.3
|
663.5
|
1.15
|
0.26
|
160.57
|
673.8
|
675.0
|
1.20
|
0.17
|
0.25
|
Geophysics
In November 2023, a geophysical
Pole-Dipole Induced Polarisation ("IP") survey was initiated to
facilitate the identification of deeper targets. The data was
obtained from five northwest-southeast oriented IP profiles, which
were broadly perpendicular to the structures in the area which are
oriented in a broadly north-south direction (Figure 1). The survey encompassed a
12.05 km total length with 200-metre line spacing. Electrodes were
positioned at 50-metre intervals, utilising a mixed array type of
surveying. The survey equipment comprised a Canada GDD TxII-5000W
transmitter and a France Iris Elrec Pro 10 receiver operating in
the time domain, enabling high-resolution near-surface data
acquisition as well as lower-resolution deeper signal detection.
Survey parameters were optimised for depths of up to 500 metres.
While three lines were completed in November 2023, the remaining
two lines were finalised in April 2024 due to adverse weather
conditions over the winter, including heavy rain and
snow.
Upon the conclusion of the data
processing and interpretation (Figure 3), two geophysical structural
systems, oriented northeast-southwest, were defined and noted to be
running broadly parallel to the mapped geology. In the
central portion of the project area, resistivity anomalies with low
to moderate values are observed. This segment of the
geophysical profiles exhibit high chargeability values.
Analysis of drill results in these locations indicates the
presence of low-grade disseminated sulphide minerals to significant
depths.
No drilling has been conducted in
the western region of the geophysical profiles to date. The
geophysical resistivity and chargeability results indicate
coincident high resistance and high chargeability values in this
area, representing a significant target for potential
mineralisation. Drilling will be targeted in this area in future
drilling programmes.
Figure 3: Resistivity (above)
and chargeability (below) results of the Hizarliyayla geophysics in
3D, with anomaly of interest on the western flank shown within a
black ellipse.
Downhole Geochemistry
Multi-element results were obtained
from all samples submitted to the laboratory. As part of the
multi-element analyses, PCA ("Principal Component Analysis") and
SOM ("Self Organising Maps") analysis were applied to the data to
define clusters. At Hizarliyayla, 8
clusters were defined, differing from each other in terms of
dominant elements, element concentrations and element correlations.
The dominant lithology at Hizarliyayla is andesite, with various
alteration intensities and zones observed. This clustering study
has helped to add definition to the boundaries of the alteration
zonation, helping to define further drill targets.
The study has emphasised the
difference in alteration across the area of Hizarliyayla
drill-tested to date. The alteration zones are defined clearly,
although at varying intensities, with sericite and albite dominant
in the west and illite and chlorite dominant in the east,
suggesting an increase in the system's temperature to the
northwest. There is a third, smaller zone in the north
characterised by potassic alteration. The more intense
illite-chlorite alteration is seen in an area containing more
abundant disseminated pyrite, matching the observations made from
the geophysical profiles. A cluster representing the
mineralised intervals is seen amongst all the alteration
domains.
Sampling and Assaying Procedures
All diamond drill core is currently
being processed at the Ardanuc depo facility in Artvin and analysed
at the Kiziltepe Mine Laboratory. HQ-size drill-core samples
from the drilling programme at Hizarliyayla were cut in half by a
diamond saw and sent for analysis in batches in line with the
Company's quality control procedures. Core recovery for all
drilling conducted at Hizarliyayla during this campaign was
82%.
To date, a total of 6,970 sample
results for 6,737 metres of sampled drill core has been returned
from the KML (plus 1,405 QA/QC samples). So far, 6% of all
analysed samples have also been analysed by ALS Global in Izmir as
an external laboratory check as part of the QA/QC procedures used
for the project, with a 10% check rate to be achieved by the end of
the drilling programme.
QA/QC sample insertion rates vary
depending on the batch size accepted by the laboratory. During the
2021-2023 drilling, Zenit QA/QC protocol required 1 blank, 1 CRM, 1
field duplicate, 1 pulp duplicate and over 10% samples analysed at
an external laboratory. Since October 2022, KML has been
accredited by the Turkish Accreditation Agency (TÜRKAK) with 'TS EN
ISO/IEC 17025:2017 General Requirements for the Competence of
Experimental and Calibration Laboratory'.
All samples were assayed for gold
using a 30g fire assay. Multi-element ICP was used for
copper, lead, molybdenum, and zinc analyses. Reviews of the
assay results have determined that all Quality Control and Quality
Assurance samples (blanks, standards, and duplicates) passed the
required quality control checks established by the Company, with
duplicate samples showing excellent correlation. Laboratory
sample preparation, assaying procedures and chain of custody are
appropriately controlled. Zenit maintains an archive of
half-core samples and a photographic record of all cores for future
reference.
Contacts:
Ariana Resources plc
|
Tel: +44 (0) 20 7407 3616
|
Michael de Villiers,
Chairman
|
|
Kerim Sener, Managing
Director
|
|
Beaumont Cornish Limited (Nominated Adviser)
|
Tel: +44 (0) 20 7628 3396
|
Roland Cornish / Felicity
Geidt
|
|
Panmure Liberum (Joint Broker)
|
Tel: +44 (0) 20 7886 2500
|
Kieron Hodgson / Atholl Tweedie /
Rauf Munir
|
|
Zeus Capital Limited (Joint Broker)
Harry Ansell / Katy Mitchell /
George Krokos
Yellow Jersey PR Limited (Financial PR)
|
Tel: +44 (0) 203 829 5000
Tel: +44 (0) 7983 521 488
|
Dom Barretto / Shivantha Thambirajah
/
Bessie Elliot
|
arianaresources@yellowjerseypr.com
|
Beaumont Cornish Limited ("Beaumont Cornish") is the Company's
Nominated Adviser and is authorised and regulated by the FCA.
Beaumont Cornish's responsibilities as the Company's Nominated
Adviser, including a responsibility to advise and guide the Company
on its responsibilities under the AIM Rules for Companies and AIM
Rules for Nominated Advisers, are owed solely to the London Stock
Exchange. Beaumont Cornish is not acting for and will not be
responsible to any other persons for providing protections afforded
to customers of Beaumont Cornish nor for advising them in relation
to the proposed arrangements described in this announcement or any
matter referred to in it.
Editors' Note:
The information that relates to
Exploration Results is based upon information compiled by Ruth
Woodcock, Exploration Group Leader, Ariana Resources plc. Ruth
Woodcock is a member of Recognised Professional Organisations as
defined by JORC 2012: a Chartered Geologist (CGeol, Geological
Society of London) and European Geologist (EurGeol, European
Federation of Geologists) and has sufficient experience which is
relevant to the style of mineralisation and type of deposit under
consideration and to the activity upon which she is reporting as a
Competent Person as defined in the 2012 Edition of "The
Australasian Code for Reporting of Exploration Results, Mineral
Resources and Ore Reserves." Ms. Woodcock consents to the inclusion
in this report of the matters based on the information compiled by
her, in the form and context in which it appears.
The information in this announcement
that relates to exploration results is based on information
compiled by Dr. Kerim Sener BSc (Hons), MSc, PhD, Managing Director
of Ariana Resources plc. Dr. Sener is a Fellow of The Geological
Society of London and a Member of The Institute of Materials,
Minerals and Mining and has sufficient experience relevant to the
styles of mineralisation and type of deposit under consideration
and to the activity that has been undertaken to qualify as a
Competent Person as defined by the 2012 edition of the Australasian
Code for the Reporting of Exploration Results, Mineral Resources
and Ore Reserves (JORC Code) and under the AIM Rules - Note for
Mining and Oil & Gas Companies. Dr. Sener consents to the
inclusion in the report of the matters based on his information in
the form and context in which it appears.
About Ariana Resources:
Ariana is an AIM-listed mineral
exploration and development company with an exceptional
track-record of creating value for its shareholders through its
interests in active mining projects and investments in exploration
companies. Its current interests include a major gold development
project in Zimbabwe, gold production in Türkiye and copper-gold
exploration and development projects in Cyprus and
Kosovo.
Ariana owns 100% of the Dokwe Gold Project ("Dokwe") in
Zimbabwe. Dokwe is made up of the Dokwe North and Dokwe
Central gold deposits which are located in the Tsholotsho District
near the city of Bulawayo. The deposits have a combined JORC
Measured, Indicated and Inferred Resource of over 1.83 million
ounces of gold (as at June 2024) and the project represents the
largest undeveloped gold project in Zimbabwe.
The Company holds 23.5% interest
in Zenit
Madencilik San. ve Tic. A.S. a joint venture with Ozaltin
Holding A.S. and Proccea Construction Co. in Türkiye which contains
a depleted total of c. 2.2 million ounces gold equivalent (as at
March 2024, using a price ratio of 90 Ag to 1 Au). The joint
venture comprises the Kiziltepe Mine and the Tavsan and Salinbas
projects.
The Kiziltepe Gold-Silver
Mine is
located in western Türkiye and contains a depleted JORC Measured,
Indicated and Inferred Resource of 171,700 ounces gold and 3.3
million ounces silver (as at March 2024). The mine has been in
profitable production since 2017 and has been producing at an
average rate of c.22,000 ounces of gold per annum. A Net Smelter
Return ("NSR") royalty of 2.5% on production is being paid to
Franco-Nevada Corporation.
The Tavsan Gold
Mine is
located in western Türkiye and contains a JORC Measured, Indicated
and Inferred Resource of 311,000 ounces gold and 1.1 million ounces
silver (as at March 2024). Following the approval of its
Environmental Impact Assessment and associated permitting, Tavsan
is being developed as the second gold mining operation in Türkiye
and is currently in construction. A NSR royalty of up to 2% on
future production is payable to Sandstorm Gold.
The Salinbas Gold
Project is
located in north-eastern Türkiye and contains a JORC Measured,
Indicated and Inferred Resource of 1.5 million ounces of gold (as
at July 2020). It is located within the multi-million ounce Artvin
Goldfield, which contains the "Hod Gold Corridor" comprising several
significant gold- copper projects including the 4 million ounce Hod
Maden project, which lies 16km to the south of Salinbas. A NSR
royalty of up to 2% on future production is payable to Eldorado
Gold Corporation.
Ariana owns 76% of
UK-registered Western Tethyan Resources Ltd ("WTR"), which operates across
south-eastern Europe and is based in Pristina, Republic of Kosovo.
The company is targeting its exploration on major copper-gold
deposits across the porphyry-epithermal transition. WTR is being
funded through a five-year Alliance Agreement with Newmont Mining
Corporation (www.newmont.com) and is separately earning-in to up to
85% of the Slivova Gold Project.
Ariana owns 61% of
UK-registered Venus Minerals PLC ("Venus") which is focused on
the exploration and development of copper-gold assets in Cyprus
which contain a combined JORC Indicated and Inferred Resource of
16.6Mt @ 0.45% to 0.80% copper (excluding additional gold, silver
and zinc.
Ariana owns several investments in
listed and private companies via its Australian subsidiary
Asgard Metals Pty. Ltd. ("Asgard"), which also provides technical input into the
various investee company exploration programmes. Investments
have been made in high-value potential, discovery-stage mineral
exploration companies located across the Eastern Hemisphere and
within easy reach of Ariana's operational hubs in Australia,
Türkiye, UK and Zimbabwe. Its most advanced interest is
through a 5.5% holding of Panther Metals Limited (ASX:
PNT).
Panmure Liberum Limited and Zeus
Capital Limited are brokers to the Company and Beaumont Cornish
Limited is the Company's Nominated Adviser.
For further information on Ariana,
you are invited to visit the Company's website at
www.arianaresources.com.
Glossary of Technical Terms:
"Ag" chemical symbol for
silver;
"Au" chemical symbol for
gold;
"Cu" chemical symbol for
copper;
"g/t" grams per tonne;
"IP" Induced
Polarisation;
"KML" Kiziltepe Mine
Laboratory;
"m" Metres;
"PCA" Principal Component
Analysis;
"Pb" chemical symbol for
lead;
"ppm" parts per million;
"Zn" chemical symbol for
zinc.
Ends.