OTCPK:NOSOF - Post by User
Comment by
hrockon Apr 06, 2008 8:08am
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Post# 14942890
Chromite vs Ni - VMS vs MMS - Aucon
Chromite vs Ni - VMS vs MMS - Auconeh....AuCon,
Seems both Chromite or NI can be either VMS or magmatic.............assa in below postin'.
Neverdaless, findin' Chromite beds, inna mo' dan one place, whether stood onna end or not..........indicates possible Platinum Group Metals..............Platinum.............anna da whole mess o' ...iums ..........includin' rhodium @ $6000 per oz.
Metinks...........dis issa good fo' some excitement...............get set fo' a news release next week from SPQ/KWG drillin' der FWR option...............previous chromite hit!
Just da way I see dat!
HardRock
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That's a nice !!!!
Chromite is VMS - volcanic, nickel is magmatic - intrusive.
VMS was always known at McFaulds. Magmatic is just recently known -- Double Eagle. Not related !!!! Apples and oranges. LOL.
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Rock Speculation - Chromite Means PGM!!!
Just da way I see dat!
HardRock
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"- Further drilling at Eagle Two (Anomaly AT2) continues to trace a Shear Hosted Sulphide ("SHS") zone containing bands of massive sulphide mineralization with visible copper-nickel minerals from the Precambrian rock surface (starting at 10 meters below surface) to 190 meters below surface where the approximately up to 21 meters thick, 75 meters long oval-shaped mineralized zone is within 30 meters of the favourable underlying granodiorite intrusive contact. - Massive Chromite beds up to 48.4 meters in core thickness at AT2 have been encountered in the near vertical dipping, wide peridodite sill occupying the non-conformity between the underlying granodiorite intrusive to the north and overlying Precambrian volcanic stratigraphy to the south." The Eagle 2 description in the NR starts to draw some similarities in my mind to the geological settings of a world class PGM mining district - The Stillwater Complex in Montana. The Stillwater Complex, which hosts two of the largest PGM producing mines in NA, is a Layered Igneous Complex which is composed of a succession of ultramafic to mafic rocks derived from a large complex magma body. The molten mass was sufficiently large and fluid to allow its chemical constituents to crystallize slowly and sequentially, with the heavier mafic base-metal minerals settling more rapidly toward the base of the cooling complex, and PGM-enriched host rock representing one layered sequence. The layered, mineralized body was pushed by a later ground movement to have turned about 70 degrees to become The Stillwater Complex. Bushveld, the world's biggest PGM producer, with its Bushveld Complex, has a similar geological setting. The geological model of The Stillwater Complex was a brainchild of the famed geophysicist Terry Crebs, who also initiated the correct theory that helped the early development of Voisey's Bay discovery (pp. 108-109, The Big Score) This, of course is purely my imagination at this point. ~p |