
TNR Gold Corp (TNR) is
pleased to announce the acquisition of the Mavis Lake Project.
The project encompasses nine identified rare-element bearing pegmatites
within a 32 hectare claim block. The
property is located approximately 15km northeast of the town of Dryden, Ontario
and is road accessible.
TNR has staked the property
with the intent to further define the known lithium, tantalum and related
rare-element showings on the property.
The Mavis Lake Project
covers the eastern extent of the Mavis Lake pegmatite group, an east-trending
concentration of rare-element-bearing pegmatites and related metasomatic zones.
The nine known pegmatites on the property are denoted as Pegmatite 11
through to Pegmatite 19 respectively.
The pegmatites are a mix of albite-spodumene-type and albite-type
pegmatites (Breaks, 2003).
Lithium and tantalum values
to note in Mavis Lake albite-type pegmatites are:
|
Pegmatite No
|
Sample Number
|
Li2O
|
Ta (ppm)
|
Sample type
|
|
Pegmatite 13
|
244
|
2320 ppm over 1.3 m
|
170
|
Channel cut
|
|
Pegmatite 14
|
245
|
250 ppm over 0.63 m
|
70
|
Channel cut
|
|
Pegmatite 15
|
246
|
1980 ppm over 1.7 m
|
150
|
Channel cut
|
|
Pegmatite 19
|
247
|
225 ppm
|
280
|
Grab sample
|
(Breaks, email 2009)
Lithium Mineralization:
Pegmatites 11, 12, 17 and 18, have been
classified as albite-spodumene-type pegmatites.
This type of pegmatite typically contains the highest spodumene [LiAl(Si2O6)]
content of any pegmatite type (Breaks, email 2009). Pegmatite 18 contains 53%
volume spodumene (Breaks Ph.D. thesis 1989, p. 104).
Tantalum Mineralization:
Tantalum-bearing minerals were confirmed
in albite-type and albite-spodumene pegmatites on the Mavis Lake property by 94
electron microprobe analysis. These minerals were verified as Mn-tantalite,
Mn-columbite and wodginite group [(Mn(Sn,Ta)Ta2O8] (2003
Ontario Geological Survey MRD 127).
'Wodginite is the chief ore mineral for
tantalum at the world-famous Tanco pegmatite in SE Manitoba and hence the
presence of this rare mineral group in the Mavis Lake claim-block underscores
the exploration potential for tantalum' (Breaks, email 2009).
Additional mineralization to
note is the presence of the tungsten ore, scheelite [Ca(WO4)] in vein
systems proximal to Pegmatites 13, 14 and 16, as well as beryl in Pegmatites 13,
14 and 15 (Breaks, 1989).
The Mavis Lake Project contains known
lithium and tantalum bearing pegmatites.
TNR plans to investigate the showings to further outline the economic
potential of the property.
|