5 Nov 2008 07:00
ο»Ώ
www.tertiaryminerals.com
Β 5 NovemberΒ 2008
Β
Β
Β
Tertiary Minerals plc ("Tertiary" or "the Company") is pleased toΒ reportΒ thatΒ secondΒ round assayΒ results fromΒ drill coreΒ haveΒ revealedΒ widerΒ intervals ofΒ fluorsparΒ mineralisationΒ atΒ its 100% owned Storuman fluorspar deposit in the VΓ€sterbotten district of Northern Sweden.Β
The results ofΒ theΒ first roundΒ ofΒ assays,Β released in early September,Β confirmed that the StorumanΒ fluorsparΒ depositΒ extends for at least 2 km alongΒ strike andΒ that the mineralisationΒ isΒ also present inΒ peripheralΒ areasΒ not considered during the 1970s exploration.Β Β These assays, however,Β as with assays in the 1970s, wereΒ mainlyΒ restricted toΒ the horizontally bedded lower sandstone horizonΒ whereΒ the extensiveΒ fluoriteΒ mineralisation wasΒ confirmed to be present in visually significant amountsΒ as a distinctive lilac coloured fluorite.Β
A second round of assaying hasΒ nowΒ confirmedΒ the Company's suspicion that pale-colouredΒ Β fluoriteΒ also occurs in the immediatelyΒ overlyingΒ quartzite horizonΒ andΒ it'sΒ flanking transitional zonesΒ which were, in many cases, not originally selected for assayΒ as it is difficult to seeΒ theΒ pale coloured fluorite against theseΒ pale-coloured host rocks.Β
The tableΒ belowΒ showsΒ the significant results from theΒ secondΒ roundΒ ofΒ assays.Β TheΒ threeΒ left-handΒ columnsΒ show the newly assayed intervals. TheΒ middle three columns show various re-calculated intersections where the new assay results areΒ included with previously reportedΒ adjacentΒ assay intervals and the threeΒ right-handΒ columns show theΒ first round assayΒ results reported on 2 SeptemberΒ 2008Β for comparison.
Some of the holes were drilled at too low an elevation for theΒ pale fluorsparΒ mineralisedΒ upperΒ strataΒ to be intersected and in some cases, where intersected,Β theseΒ upperΒ horizonsΒ have notΒ yet been sampled for assay.Β
Tertiary'sΒ ChairmanΒ Patrick CheethamΒ commented: "The results areΒ really quiteΒ significant,Β with individual mineralised intervals up to 43% thicker andΒ withΒ up to 20% higher grade thanΒ shown byΒ first round assaysΒ alone. NotΒ only do they point to further tonnage potential in an already large mineralised system, butΒ someΒ of theΒ nearer-surfaceΒ material previouslyΒ considered asΒ mineΒ wasteΒ inΒ 1970sΒ pit designsΒ could now be consideredΒ ore."
The newΒ assayΒ results will be incorporated into the geological model being developed for the Scoping StudyΒ which is currentlyΒ in progress.Β
The concept being developed by the Company is a mining operation producing at least 100,000 tonnes per annum of acid grade fluorspar. The world market for fluorspar is just over 5 million tonnes per annum of which 65% is for acid grade fluorspar. Published prices for acid grade fluorspar have climbed in the past year from US$270 toΒ the current level ofΒ US$580 due to shortages of supply from traditional Chinese sources.Β
A drill hole location plan is available on the Company's website atΒ www.tertiaryminerals.com.
Background
Tertiary was awarded the Storuman exploration licence in JanuaryΒ 2008. The Storuman fluorite deposit is located in an area with well established infrastructure. It is located adjacent to a sealed highway 20km from the regional town ofΒ StorumanΒ which is connected by road and rail to the city andΒ portΒ ofΒ UmeΓ₯Β on theΒ Gulf of Bothnia. In the other direction the highway leads to theΒ port city ofΒ Mo-i-RanaΒ inΒ Norway.
The StorumanΒ mineralisationΒ was last evaluatedΒ in the 1970s by GrΓ€nges Aluminium who calculated an "ore reserve"* of 12.5 million tonnes grading 13.3% CaF2.Β (CaF2 is the chemical formula for the mineral fluorite, known commercially as "Fluorspar"). This "ore-reserve" is historic and not compliant with any recognised resource or reserve code.
Fluorspar is the main industrial source of fluorine for the manufacture of hydrofluoric acid and derivative fluorine chemicals including refrigerants, PTFE (Teflonβ’) and aluminium hydrofluoride, a flux used in the reduction of alumina to aluminium. It is also used as a flux in steel making, in the ceramics industry and in the manufacture of nuclear fuel (uranium hexafluoride).
Fluorspar consumers, several of which are based in Europe, are facing critical supply shortages as traditional supplies fromΒ ChinaΒ are diverted to meet growing Chinese domestic demand.Β ChinaΒ has recently imposed export quotas and export taxes to discourage export and thus ensure domestic supplies.Β
Further info:
Patrick Cheetham, Executive Chairman, Tertiary Minerals plc.Β Tel: +44 (0)1625-626203
Ron Marshman/John Greenhalgh,Β Lothbury Financial. Tel: +44(0)20-7011 9411Β
Jonathan Wright, Seymour Pierce Limited.Β Tel:Β +44(0)20-7107-8000
Notes:
The information in this release has been compiled and reviewed by Mr.Β Patrick CheethamΒ (MIMMM, MAusIMM) who is a qualified person for the purposes of the AIM Guidance Note for Mining Oil & Gas Companies issued on March 16, 2006. Mr Cheetham is a Member of the Institute of Materials, Minerals & Mining and also a member of the Australasian Institute of MiningΒ & Metallurgy.
Drill holes being reported are vertical and theΒ mineralisation intersected is believed to beΒ horizontal. ConsequentlyΒ theΒ reported down-hole intersected thickness will approximate true thicknesses.
TableΒ Of Significant Drill Intersections (SecondΒ Round Assay Results)Β
|
AdditionalΒ (2ndΒ Round)Β Assay Results |
Revised Composite Intervals |
Original reported Intervals |
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|
Drill HoleΒ Number |
From (Depth Down-Hole)Β (m=metres) |
Drill Assay Interval (m=metres) |
Assay ResultsFluorspar (CaF2)Β % |
From (Depth Down-Hole)Β (m=metres) |
Drill Assay Interval (m=metres) |
Assay ResultsFluorspar (CaF2)Β % |
From (Depth Down-Hole)Β (m=metres) |
Drill Assay Interval (m=metres) |
Assay ResultsFluorspar (CaF2)Β % |
|
Β |
Β |
Β |
Β |
||||||
|
08TS001 |
Previous assays fromΒ bedrock surfaceΒ (Sandstone), Quartzite & Transition Zones not present at this low elevationΒ |
14.30m |
1.25m |
12.1% |
|||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS002 |
Low grade fluorsparΒ from bedrock surface (Quartzite)Β above originally reportedΒ high grade Lower Transition ZoneΒ |
13.50m |
7.00m |
10.0% |
|||||
|
includes |
13.50m |
2.80m |
13.3% |
||||||
|
Includes |
18.80m |
1.70m |
13.3% |
||||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS003 |
9.40m |
5.00m |
17.8% |
9.40m |
16.50m |
12.9% |
14.40m |
11.50m |
10.8% |
|
IncludesΒ |
9.40m |
6.15m |
17.2% |
14.40m |
1.15m |
14.4% |
|||
|
Includes |
20.40m |
1.90m |
12.9% |
||||||
|
Includes |
23.70m |
2.20m |
16.6% |
||||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS004 |
52.30m |
1.50m |
10.2% |
60.25m |
4.35m |
13.5% |
|||
|
Β |
Β |
Β |
Β |
||||||
|
08TS005 |
5.60m |
3.60m |
13.9% |
5.60m |
13.90m |
13.3% |
9.20m |
10.30m |
13.1% |
|
Includes |
14.80m |
4.70m |
19.2% |
||||||
|
Includes |
16.30m |
3.20m |
22.7% |
||||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS006 |
PreviousΒ reportedΒ assays fromΒ Quartzite, Lower Transition & Sandstone.Β 3mΒ UpperΒ Transition Zone notΒ yetΒ sampledΒ |
11.50m |
18.05m |
10.6% |
|||||
|
Includes |
11.50m |
3.35m |
21.5% |
||||||
|
Includes |
25.15m |
4.40m |
15.5% |
||||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS007 |
10.05m |
2.20m |
6.8% |
25.10m |
2.75m |
16.7% |
|||
|
Includes |
Mineralised from bedrock surfaceΒ (Upper Transition Zone) |
||||||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS008 |
Planned but not drilled |
Β |
Β |
||||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS009 |
23.95m |
4.05m |
9.5% |
23.95m |
5.85m |
10.8% |
28.00m |
1.80m |
13.9% |
|
and |
4m UpperΒ Transition Zone notΒ yet sampled |
37.10m |
1.30m |
16.5% |
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|
Β |
Β |
Β |
Β |
||||||
|
08TS010 |
6m UpperΒ Transition Zone notΒ yet sampled |
26.95m |
5.50m |
5.1% |
|||||
|
Β |
Β |
Β |
Β |
||||||
|
08TS011 |
Previous assays fromΒ complete Upper Section, Hole finished in mineralised Sandstone |
27.20m |
1.75m |
12.8% |
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