Empire
Metals Limited / LON: EEE / Sector: Natural Resources
24 October 2024
Empire Metals
Limited
("Empire" or "the Company")
Diamond
Drilling at Pitfield Completed
Titanium-rich Weathered Cap Significantly Thicker than
Anticipated
Empire Metals Limited (LON:
EEE), the AIM-quoted resource exploration
and development company, is pleased to
announce that the diamond core drilling programme at the Pitfield
Project ('Pitfield'),
located in Western Australia, has been completed, identifying new
extensive, thick zones of strongly weathered "saprolite" cap.
Samples will be used primarily for metallurgical testwork and
flowsheet development as well as informing the plans for further
diamond core and reverse circulation ('RC') drilling aimed at
defining a maiden Mineral Resource Estimate ('MRE') in 2025.
Highlights
· Diamond core drill
programme completed on schedule, with five holes drilled to planned
depths at both the Thomas and Cosgrove Exploration Target areas for
a total of 679 metres.
· All drill holes
encountered extensive weathered zones from very near surface
to depths of around 60 metres, nearly double that
previous encountered at the Cosgrove and Thomas prospects,
confirming the extremely soft and friable nature of the bedded
sandstones in this weathered zone.
· These significantly
deeper intercepts of weathered sandstones at both target areas bode
well for the development of a large scale Mineral Resource Estimate
for the higher-grade, high-purity anatase-rich weathered
cap.
· Excellent recovery
of core was achieved which will primarily be used for metallurgical
testwork and process flowsheet development including:
o standard hardness and
grindability tests to determine the energy input needed to liberate
the titanium-bearing minerals from gangue minerals contained in the
rocks; and
o bulk composites of the
weathered zone for mineral separation and titanium extraction
testwork.
· The key observation
from core logging is that the material characteristics of these
highly weathered bedded sandstones will mean easier mining
conditions and significantly less energy consumption required
for comminution.
· With the completion
of this diamond core drilling programme the Company has now drilled
100 RC holes for a total of 14,988m and 17 diamond core holes for a
total of 2,704m.
Shaun Bunn, Managing Director, said:
"I am pleased to
provide an update on what has been an extraordinarily successful
diamond drill campaign. Core logging has confirmed the extensive
depth of weathering, well over 60 metres from surface in the zones
targeted, where our geoscientists had predicted they would be based
on the previous drill sample logging and geochemical assay results.
This logging data will help verify the geological model used for
the Exploration Target estimates (announced 12 June 2024) and allow
us to reduce our search area radius for high-grade, anatase rich
mineralisation and hence reduce the size and cost of the next phase
of drilling ahead of defining a maiden MRE.
"Furthermore, the
excellent recovery of drill core achieved throughout the campaign
ensures that we have more than sufficient representative samples of
the weathered zone to accelerate the mineral separation testwork.
Gravity testwork is continuing on previously collected samples of
the fresh bedrock throughout October and November, in order to
evaluate the effect of grind size on particle liberation and to
produce mineral concentrate samples for preliminary
hydrometallurgical testing. Other mineral separation processes
being assessed include magnetic separation and froth flotation. As
soon as the weathered core samples from this campaign are
available, expected within weeks, a duplicate mineral separation
testwork programme will commence."
Observations and
Logging Results from Diamond Core Programme September-October
2024
The current diamond core drilling programme has been
completed, with a total of ten diamond core drill holes at the
Thomas and Cosgrove Prospects, identifying extensive weathered
material for analysis (Figure 1). This drilling has provided
invaluable geological insight into the weathering profiles at both
prospects, confirming the depth of weathering, and identifying
various aspects of the weathered profile including the intensity of
the weathering and structures within the weathered rock mass.
Figure 1: Grey
scale magnetics map overlain by airborne gravity results with the
location of all drillholes and the ten recently drilled diamond
core drillholes highlighted by blue diamonds.
The weathering profiles vary across both prospects,
which is to be expected. The data collected from the core logging
will significantly improve the current geological model's
weathering profile and allow the thickness and intensity of
weathering to be tied back to the geochemical and mineralogical
results. This will allow the exploration team to focus the next
drill campaign on defining areas of high-grade, high-purity
anatase-rich mineralisation and help reduce the size and cost of
drilling ahead of defining a maiden MRE.
The geological observations from the drill core
collected across both prospects have identified that under thin
lateritic or soil cover lies an intensely weathered zone where the
original rock mass has been completely altered to saprolite.
All elements of the original rock type, whether sandstone,
conglomerate or siltstone have been altered, with an abundance of
cream-coloured kaolinite now present. Lying beneath this saprolite
are weathered and partially weathered basement rocks, being the
more recognisable sandstones, siltstones and conglomerates seen
throughout the sedimentary basin. The weathered rocks within
this zone are extremely friable and tend to be incredibly soft,
with a knife easily inserted into the drill core. The
hardness and strength of the rock increases with depth as the
profile transitions out of the weathered zone into the partly
weathered, transitional zone. Ultimately the partly weathered
profile transitions into fresh bedrock, generally over a width of
several metres, and here the rocks become stronger and the drill
core becomes more competent.
Figure 2. Diamond
Core drilling at the Thomas Prospect.
A notable difference between the Cosgrove and Thomas
prospects is that the intensity of weathering is stronger at the
Thomas property with slightly thicker, more consistent saprolite
and generally deeper weathering (Figure 3). There are zones
at Cosgrove that show these characteristics, however these are on
the western margin of the prospect where it has been drilled.
Figure 3: Cross
Section from Thomas Prospect showing weathered cap profile (refer
Figure 1 for Section A-B from 6724500N.)
Diamond Core results
from Thomas Exploration Target
There were five diamond holes drilled for 367.8m
across the Thomas prospect. The initial four holes were
drilled to evaluate the central zone where the better RC results in
the weathered profile were previously identified. These four
holes (DD24TOM004-DD24TOM007) were designed to map the weathering
profile from east to west and north to south to determine the depth
of weathering, the intensity of weathering and the thicknesses and
structure of the various weathering zones.
Each of the four holes have a laterite cover which
extends between 6-14m from surface. Previous drilling has shown
that this laterite cover is titaniferous. Logging of the four holes
shows that the depth of weathering on the western side of the
prospect is greater than the eastern side, with a thicker
saprolitic profile ranging between 50-54m being some 10-12m greater
than that observed on the eastern side. This closely fits the data
from the previous RC drilling which also shows a decrease in
thickness of weathering to the south.
Figure 4: DD24TOM004
showing saprolite at top of hole before transitioning into
extremely weathered sandstone (4.6m - 16.4m).
Hole DD24TOM008 was drilled to assess the weathering
profile between two RC holes that intercepted high-grade
mineralised zones of weathered sandstone, RC24TOM002 and
RC24TOM003.
The diamond core hole from this programme intercepted
14m of saprolite at the top and cut the base of the weathering at
58m. This depth is approximately 10m deeper than the RC holes,
based on empirical observation which will need to be confirmed with
geochemical data.
Structural data at the Thomas Exploration Target
indicates that the beds are dipping between 30 and 50 degrees to
the southeast, the same as observed from previous drilling.
Table 1: Diamond
Core Drill Holes and Weathered Zone Profiles for Thomas
Prospect
Hole ID
|
Total Metres
Drilled
|
Highly Weathered
Zone (m range)
|
Highly Weathered
Zone (total metres)
|
Comments
|
DD24TOM004
|
75.4m
|
6m to 56m
|
50m
|
Laterite cap to 6m
|
DD24TOM005
|
81.4m
|
6m to 60m
|
54m
|
Laterite cap to 6m
|
DD24TOM006
|
72.6m
|
5m to 58m
|
53m
|
Laterite cap to 5m
|
DD24TOM007
|
65.8m
|
14m to 57m
|
43m
|
Laterite cap to 14m
|
DD24TOM008
|
72.6m
|
1m to 58m
|
57m
|
Soil cover
|
Total
|
367.8m
|
|
|
|
Diamond Core results
from Cosgrove Exploration Target
There were five diamond holes drilled for 311.2m
across the Cosgrove prospect. There were four holes
(DD24COS005-DD24COS007) drilled to evaluate the northerly zone and
one drill hole (DD25COS004) was designed to assess the western
margin of known weathered mineralisation. All five drill
holes were designed to map the weathering profile across the
prospect to determine the depth of weathering, the intensity of
weathering and the thicknesses and structure of the various
weathering zones.
The four holes drilled in the north identified 5-14m
of saprolite below a laterite cap. The depth of weathering is
between 39-55m. Hole DD24COS004 intersected 11m of saprolite and
52m of underlying weathered bedrock. The depth of weathering is
more variable at Cosgrove from south to north and east to west. The
geochemical data from these holes will be instructive to
understanding the link between the weathering profile and
grade.
Figure 5: DD24COS005 showing
smaller saprolite zone before transitioning into extremely
weathered sandstone (7.3m - 17.1m).
Table 2: Diamond
Core Drill Holes and Weathered Zone Profiles for Cosgrove
Prospect
Hole ID
|
Total Metres
Drilled
|
Highly Weathered
Zone (m range)
|
Highly Weathered
Zone (total metres)
|
Comments
|
DD24COS004
|
78.7m
|
11m to 63m
|
52m
|
Laterite cap to 11m
|
DD24COS005
|
48.7m
|
0m to 45m
|
45m
|
Drilled in to weathered bedrock
|
DD24COS006
|
48.4m
|
1m to 44m
|
43m
|
Soil cover
|
DD24COS007
|
62.7m
|
1m to 50
|
49m
|
Soil cover
|
DD24COS008
|
72.7m
|
1m to 60m
|
59m
|
Soil cover
|
Total
|
311.2m
|
|
|
|
Ongoing and Planned
Metallurgical Testwork
Metallurgical drill core will be used to further the
process flowsheet development work. This drill campaign has
provided samples in both weathered and fresh zones of the
mineralisation.
Samples will be used for a range of tests
including:
-
Individual intervals for standard hardness and grindability
tests
-
Domain / zone based bulk composites for mineral separation and
titanium extraction testwork.
The hardness and grindability testwork will provide
information on energy input needed to liberate the titanium-bearing
minerals from gangue minerals contained in the rocks. In particular
the technical team are looking to understand how the rocks break
and the difference between the weathered and fresh rock in terms of
energy required to achieve liberation. This information will guide
equipment selection, cost of processing and give an early
indication of variability within the mineralisation.
Understanding variability will assist in sample
selection and number of samples that should be tested in the next
phases of the studies.
Once individual samples have been tested through the
hardness and grindability process, the available samples will be
blended into larger bulk composites for mineral separation and
extraction testwork.
At this stage in the project bulk samples are used to
compare different separation techniques and test variables for each
technique ensuring that the only difference between tests is the
test itself, and not the sample being evaluated.
Both weathered and fresh rock bulk composites will be
produced, to study the metallurgical response for these
mineralisation types separately.
The treatment for these samples will build on what
has been learnt so far about the mineralisation of the Pitfield
Project. In mineral separation the key focus areas will be gravity
separation, magnetic separation and froth flotation.
Titanium extraction testwork has commenced on
preliminary concentrate samples, and whole of ore, in order to
evaluate concepts from research, literature and industry. Some of
the new samples will be used in a similar way, and some of the
sample will be reserved for a bulk run through a minerals
separation test to produce bulk mineral concentrate for
hydrometallurgical testing.
The Pitfield
Titanium Project
Located within the Mid-West region of Western
Australia, near the northern wheatbelt town of Three Springs,
Pitfield lies 313km north of Perth and 156km south of Geraldton,
the Mid West region's capital and major port. Western Australia is
ranked as one of the top mining jurisdictions in the world
according to the Fraser Institute's Investment Attractiveness Index
published in 2023, and has mining-friendly policies, stable
government, transparency, and advanced technology expertise.
Pitfield has existing connections to port (both road & rail),
HV power substations, and is nearby to natural gas pipelines as
well as a green energy hydrogen fuel hub, which is under planning
and development (refer Figure 2).
Figure 6.
Pitfield Project Location showing the Mid-West Region
Infrastructure and Services
Competent Person
Statement
The technical information in this
report that relates to the Pitfield Project has been compiled by Mr
Andrew Faragher, an employee of Eclipse Exploration Pty Ltd, a
wholly owned subsidiary of Empire. Mr Faragher is a Member of the
Australian Institute of Mining and Metallurgy. Mr Faragher 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'. Mr
Faragher consents to the inclusion in this release of the matters
based on his information in the form and context in which it
appears.
Market Abuse Regulation (MAR)
Disclosure
Certain information contained in
this announcement would have been deemed inside information for the
purposes of Article 7 of Regulation (EU) No 596/2014, as
incorporated into UK law by the European Union (Withdrawal) Act
2018, until the release of this announcement.
**ENDS**
For further information please visit www.empiremetals.co.uk or
contact:
Empire Metals
Ltd
Shaun Bunn / Greg Kuenzel / Arabella Burwell
|
Tel: 020 4583 1440
|
S. P. Angel
Corporate Finance LLP (Nomad & Broker)
Ewan Leggat / Adam Cowl
|
Tel: 020 3470 0470
|
Shard Capital
Partners LLP (Joint Broker)
Damon Heath
|
Tel: 020 7186 9950
|
St Brides Partners Ltd (Financial
PR)
Susie Geliher / Charlotte
Page
|
Tel: 020 7236 1177
|
About Empire Metals
Limited
Empire Metals is an AIM-listed
exploration and resource development company (LON: EEE) with a
primary focus on developing Pitfield, an emerging giant titanium
project in Western Australia.
Exploration activity at Pitfield has
confirmed the discovery of a new giant mineralised system extending
over 40km by 8km by 5km deep. Drilling campaigns have confirmed
high-grade TiO₂ mineralised zones across thick bedded intervals to
a vertical depth of ~350m, confirming Pitfield as a world class,
district-scale titanium mineral system.
Empire is now accelerating the
economic development of Pitfield, with the objective of becoming a
leading producer of high value titanium dioxide
products.
The Company also has two further
exploration projects in Australia; the Eclipse Project and the
Walton Project in Western Australia, in addition to three precious
metals projects located in a historically high-grade gold producing
region of Austria.