Exploration Update
Thor Mining PLC
03 October 2007
THOR MINING PLC
URANIUM EXPLORATION UPDATE
Dated: 2 October 2007
Thor Mining PLC ('the Company' or 'Thor'), AIM, ASX: 'THR' the specialist metals
company focused on advancing tungsten-molybdenum and uranium projects in the
Northern Territory of Australia, today releases an update on current exploration
activities on its uranium exploration projects in the Northern Territory of
Australia.
HIGHLIGHTS
• Reconnaissance air core drilling completed at Plenty Highway Project
with assay results expected in mid-to-late November 2007.
• Encouraging rock chip results received from ground surveys at the
Harts Range Project including elevated uranium values.
Plenty Highway Uranium Project
A program of reconnaissance air core drilling has been completed at the Plenty
Highway Uranium project in the Northern Territory, with assay results currently
awaited. A total of 16 air core holes (07PHAC001-016) were drilled for 1,582 m.
However, only 55% of the overall program was completed due to slow drilling in
difficult ground conditions. Drilling to date has completed wide spaced
reconnaissance air core holes on two north-south lines and one east-west
traverse along a fence line track.
A number of the holes did not reach bedrock due to the intersection of deep clay
horizons which exceeded the capabilities of the drill rig. At this stage, the
Company has not sourced another rig to complete more drilling.
The HoistEM data appears to have correctly defined the extent and approximate
depth of the palaeo-channels in the area. Drilling has identified a thin sandy
layer covering up to 10m of calcrete while below this thick horizons of
calcareous clay have been identified with thin units of gypsum and calcrete
being common. Anomalous scintillometer readings have been restricted to units of
quartz sand below the clays.
The most prospective area to date appears to be between holes 07PHAC010 and 012,
along the fence line traverse, where quartz sands up to 8m thick have been
identified returning twice the background radioactivity in the area. More
drilling is required in the area.
Assay results from this drilling will be available mid to late November 2007.
Harts Range Project
The Harts Range project area lies on the eastern margin of the Entia Dome. The
Entia Gneiss forms the core of the Entia Dome, which is located on the western
part of the Exploration Licence area.
In late July, a mapping and rock chip survey was carried out on tenements
EL24736 and EL24734, two of the tenements within the Harts Range Uranium Project
which is located approximately 200km east-northeast of Alice Springs in the
Arunta Province of the Northern Territory. The project includes five other
tenements, EL24827, EL24735, EL24765 and A24766.
The main objective of the sampling program was to follow up on previous rock
chips taken earlier this year from identified areas around the Mt Mary, Daicos
and Haddock prospects in order to identify drilling targets in this difficult
terrain. A number of sub-parallel pegmatites had previously been surveyed at the
Haddock Creek and Daicos prospects, with a maximum count of 19,000 cps returned.
Four samples were taken, with one 1.5kg sample returning a very high uranium
result of 8.87% U. At Mt Mary, two rock chips taken from 'hot spots' in this
area returned elevated uranium values ranging from 107 to 246ppm.
Rock chip sampling and mapping was also completed on the Daicos, Haddock, Mount
Mary (SNAF & Indiana) and Starlight prospects, with a total of 39 rock chip
samples collected.
Daicos
Reconnaissance rock chip samples taken on pegmatite veins mapped at the Daicos
prospect area returned a best assay of 19.37% U from highly radioactive samples
with visible uraninite and columbite. Other highly anomalous elements
associated with these samples included assays up to 28.32% Nb and 25.52% Ta.
Highly anomalous assays for Dy, Er, Gd, Hf, Ho, Nd, Tb, Y and Zr from these
samples were also noted. The combined average of these 9 associated rare earth
elements is 3.49%. See attached appendix for sample locations
The samples were taken along a number of contact zones associated with an
exposed pegmatite vein system covering an area of 300m by 400m. Drilling is
being planned to determine the thickness and strike extent of the individual
zones. A petrological assessment of the pegmatites is also warranted.
SAMPLE EAST NORTH PROSPECT CPS COMMENTS Th U
ID (GDA94) (GDA94)
DR001 516858 7439893 Daicos +1000 Pegmatite 0.55% 3.42%
contact
DR002 516876 7439834 Daicos +1000 Pegmatite 1.03% 9.11%
contact
DR003 516877 7439844 Daicos +1000 Pegmatite 0.67% 9.35%
contact
DR004 516894 7439851 Daicos +1000 Pegmatite 0.83% 9.85%
contact
DR005 516805 7439631 Daicos +1000 Pegmatite 1.09% 15.64%
contact
DR006 516832 7439555 Daicos +1000 Pegmatite 1.40% 18.53%
contact
DR007 516838 7439560 Daicos +1000 Pegmatite 1.48% 19.37%
contact
DR008 516874 7439418 Daicos +1000 Pegmatite 40 125
contact
DR009 516803 7439633 Daicos +1000 Pegmatite 1.23% 16.64%
contact
DR010 516701 7439604 Daicos +1000 Quartz Biotite 163 11
Gniess
DR011 516808 7439629 Daicos +1000 Pegmatite 1.18% 13.51%
contact
All units in this report are in ppm unless otherwise stated.
Haddock
The Haddock prospect covers the base of a large hill over a fold structure
containing highly radioactive epidosite altered country rock and pegmatite.
Previous trenching in the 1990's also returned highly anomalous U from trenches
across the base of the hill. Recent sampling in this area returned a best
uranium assay of 1,658 ppm from sample HK006. Additional trenching and
reconnaissance drilling is required to determine the full extent of
mineralisation in the area.
Of the 17 rock chip sample assays taken at the Haddock prospect to date, only
three exceed 0.1% uranium. The prospect should be evaluated in terms of a large
tonnage/low grade uranium resource. Haddock type anomalies have been recognised
at points along a stratigraphic arc extending north. Approximately 12 km of
prospective strike length provides potential host extensions or repetitions of
epidosite-pegmatoid layers. An detailed airborne radiometric survey should
delineate the broad corridor in which these extensions of epidosite-pegmatoid
may occur.
SAMPLE EAST NORTH PROSPECT CPS COMMENTS U(ppm)
ID (GDA94) (GDA94)
HK001 515667 7441235 Haddock +1000 Epidosite altered country 1,415
rock and pegmatoid
HK002 515667 7441235 Haddock +1000 Epidosite altered country 1,283
rock and pegmatoid
HK003 515667 7441235 Haddock +1000 Epidosite altered country 697
rock and pegmatoid
HK004 515667 7441235 Haddock +1000 Epidosite altered country 908
rock and pegmatoid
HK005 515667 7441235 Haddock +1000 Epidosite altered country 1,358
rock and pegmatoid
HK006 515667 7441235 Haddock +1000 Epidosite altered country 1,658
rock and pegmatoid
HK007 515667 7441235 Haddock +1000 Epidosite altered country 793
rock and pegmatoid
HK008 515667 7441235 Haddock +1000 Epidosite altered country 1,107
rock and pegmatoid
HK009 515694 7441305 Haddock +3000 Further east up hill 1,041
HK010 515642 7441351 Haddock +2000 Further east up hill 454
HK011 515532 7441231 Haddock n/a Western limb ex PNC 392
HK012 515535 7441226 Haddock n/a Western limb ex PNC 866
HK013 515532 7441244 Haddock n/a Western limb ex PNC 25
SL001 515150 7436830 Starlight n/a Epidosite metasomatised 331
pegmatoid
SL002 515678 7439225 Starlight n/a Gniessic metasediments at 16
contact with pegmatite
NT001 515021 7439795 Near n/a Gniessic metasediments at 9
Starlight contact with pegmatite
All units in this report are in ppm unless otherwise stated.
n/a - not applicable
Mt Mary
The newly identified Indiana prospect is associated with multiple pegmatite
intrusions in sheared country rock in a valley at the base of Mount Mary. Highly
anomalous scintillometer readings were returned from numerous samples in the
area. Further mapping, rock chip sampling, trenching and drilling will be based
on these initial rock chip assay results.
The full extent of the Indiana prospect is still not known; a best assay of
673ppm uranium was returned from initial sampling in the area.
SAMPLE EAST NORTH PROSPECT CPS COMMENTS U(ppm)
ID (GDA94) (GDA94)
MM001 532528 7452392 Mt Mary (Indiana) 800-1200 Pegmatite 112
MM002 532515 7452359 Mt Mary (Indiana) 800-1200 Pegmatite 27
MM003 532420 7452401 Mt Mary (Indiana) 800-1200 Pegmatite 184
MM004 532418 7452392 Mt Mary (Indiana) 800-1200 Pegmatite 286
MM005 532330 7452340 Mt Mary (Indiana) 800-1200 Pegmatite 44
MM006 532286 7452342 Mt Mary (Indiana) 800-1200 Pegmatite 75
MM007 532235 7452337 Mt Mary (Indiana) 800-1200 Pegmatite 410
MM008 532188 7452327 Mt Mary (Indiana) 800-1200 Pegmatite 118
MM009 532130 7452325 Mt Mary (Indiana) 800-1200 Pegmatite 196
MM010 532065 7452312 Mt Mary (Indiana) 800-1200 Pegmatite 87
MM011 530994 7452687 Mt Mary (SNAF) 800-1200 Pegmatite 451
intrusives
MM012 531020 7452644 Mt Mary (SNAF) 800-1200 Pegmatite 673
intrusives
All units in this report are in ppm unless otherwise stated.
Commenting on the latest results, Thor Mining's Chief Executive Officer, Mr John
Young said: 'With further ground based exploration in the area we believe we can
outline a number of drill targets in late stage pegmatitic intrusives within our
project areas. Of particular interest is the strong rare earth elements'
signature in the vicinity of Daicos, which upgrades the prospectivity of this
area.'
GLOSSARY OF GEOLOGICAL AND TECHNICAL TERMS
Ba The chemical symbol for the element Barium
Biotite A brown to black magnesium aluminium silicate mineral,
common in most volcanic rocks
Ce The chemical symbol for the element Cerium
Cs The chemical symbol for the element Caesium
Dy The chemical symbol for the element Dysperosium
Er The chemical symbol for the element Erbium
Epidote A yellow to green silicate mineral, formed during low
grade metamorphism or hydrothermal processes.
Felsic Descriptive of light coloured rock containing an
abundance of feldspar (generally Potassium rich) and quartz.
Hf The chemical symbol for the element Hafnium
Ho The chemical symbol for the element Holmium
Ga The chemical symbol for the element Gallium
Gd The chemical symbol for the element Gadolinium
Gneiss High grade metamorphic rock composed of alternating bands
respectively rich in light and dark coloured minerals.
Granite Light coloured, coarse-grained, intrusive igneous rock;
comprises large sections of the Earth's continental crust.
Intrusion A body of igneous rock that invades older rocks.
Mafic Descriptive of rocks containing major proportions of
magnesium and iron silicate minerals.
Mineralisation The concentration of metals and their minerals within a
body of rock.
Mineralogy The science of the study of minerals.
Nd The chemical symbol for the element Neodymium
Nb The chemical symbol for the element Niobium
Pb The chemical symbol for the metallic element Lead.
Pegmatite Very coarse-grained igneous intrusive body, usually
granitic, usually in dyke or sill form.
ppm Parts per million.
Plagioclase Plagioclase is an important rock-forming mineral and occurs
widely, primarily in igneous rocks such as basalts.
Radiometric Measurement of radiation. An airborne radiometric survey
may distinguish different rock units on the basis of their
inherent radioactive minerals.
Rock Chip Sampling Systematic collection of rock samples at a series of
different locations in order to study the distribution of
rock geochemical values.
REE Rare earth elements
Rb The chemical symbol for the element Rubidium
Scintillometer Instrument used for measuring radiation
Shear A zone in which rocks have been deformed, primarily in a
ductile manner, as a result of applied stress.
Strontium Strontium is a rare alkaline-earth metal
Structural Pertaining to geological structure; including folds,
faults, shears, cleavage, and joints. Structures range
from regional scale to microscopic.
Ta The chemical symbol for the element Tantalum
Tb The chemical symbol for the element Terbium
Th The chemical symbol for the element Thorium
U The chemical symbol for the element Uranium
Uraninite The chief ore mineral of uranium. Uraninite has the
idealized chemical composition UO2, uranium dioxide.
Thorium and rare earths, chiefly cerium, are usually
present in variable and sometimes large amounts.
Lead always is present by radioactive decay of the thorium
and uranium present
Vein A thin sheet-like intrusion into a fissure or crack,
commonly bearing quartz
Y The chemical symbol for the element Yttrium
Zn The chemical symbol for the element Zinc.
Zr The chemical symbol for the element Zirconium
JORC Compliance
The information in this report that relates to exploration results, mineral
resources or ore reserves is based on information compiled by John Young, who is
a Member of The Australasian Institute of Mining and Metallurgy. John Young is a
director of Thor Mining PLC. John Young 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 2004 Edition of the 'Australasian Code for Reporting of
Exploration Results, Mineral Resources and Ore Reserves'. John Young consents
to the inclusion in the report of the matters based on his information in the
form and context in which it appears.
Enquiries:
John Young +61 (0)419 954 020 Thor Mining PLC Chief Executive
Officer
John Simpson 020 7512 0191 ARM Corporate Finance Ltd Nominated Adviser
Leesa Peters 020 7429 6600 Conduit PR Limited Public Relations
or
Jos Simson 020 7429 6603
Nicholas Read +61 (0) 8 9388 1474 Read Corporate Public Relations/
Australia
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