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Title: Granites related to tin mineralization at Mt. Pleasant, New Brunswick, Canada: subvolcanic analogues of topaz rhyolites

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6070177

Two type of fluorine-rich (>2000 ppm F) high-silica (>74 wt. % SiO/sub 2/) granite are present in the environs of the Mt. Pleasant Tungsten Mine. Both are subvolcanic in character and Devono-Carboniferous in age. An older fine-grained granite contains biotite (+/-chlorite) and is associated with the earlier W-Mo stockwork/breccia ore bodies. It is intruded by topaz- and fluorite-bearing granite porphyry/porphyritic granite to which later Sn-polymetallic base metal mineralization appears to be related. Major element characteristics (SiO/sub 2/ > 75 wt. %; Na/sub 2/O > 3.2 wt. %; K/sub 2/O/Na/sub 2/O > 1; TiO/sub 2/ < 0.2 wt. %; CaO < 0.7 wt. %; MgO < 0.2 wt. %; P/sub 2/O/sub 5/ < 0.05 wt. %) identify both phases as anorogenic granites. Trace element contents however permit their separation and identify the later granites with Rb > 800 ppm, Li > 100 ppm, Cs > 20 ppm, Ta > 15 ppm, F > 4000 ppm, and distinctive flat REE patterns with large negative Eu anomalies as the intrusive equivalents of topaz rhyolites. Such unique REE distributions suggest that melt depolymerization resulting from the enhanced solubility of fluorine may play a pivotal role in the evolution of these felsic magmas.

Research Organization:
Carleton Univ., Ontario (Canada)
OSTI ID:
6070177
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English