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Stable isotope geochemistry and P-T-X conditions of late vein mineralization at White Pine, Michigan

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6194359
Numerous calcite veins crosscutting the main cupriferous ore zone at White Pine shed light on the late Precambrian, post-ore history of the district. Vein fluids (Na-Ca-Cl brines; 0-18% NaCl) migrated through enclosing red bed sequences and infiltrated the mineralized Nonesuch Shale, there leaching pre-existing copper (Carpenter, 1968). Based on isotopic analysis of calcites and fluid inclusion extracts, typical vein waters were evolved meteoric fluids initially sourced at high elevations SMOW = -10 to -1 percent per thousand (calculated) which presumably derived their salts by dissolution of evaporites in sediments of the Oronto Group. The carbon isotopic composition of these vein calcites typically ranges from -10 to -6 percent per thousands delta/sup 13/C PDB with rare calcite cement zones possessing anomalously depleted values (-31 percent per thousands). Such depleted values indicate a significant contribution of carbon derived from the oxidation of organic matter a process which may also account for the anomalously light delta D (-93 percent per thousands) composition of some inclusion waters. Integration of several types of evidence indicates vein fluid temperatures were between 50 - 93/sup 0/C, and at times during calcite precipitation, total hydrostatic pressures were certainly below 400 bars and probably below 200 bars. These pressures require erosional removal of the entire Jacobsville Sandstone and a substantial part of the Freda Sandstone before the vein mineralization came to a close in late Precambrian time.
Research Organization:
Univ. of Michigan, Ann Arbor (USA)
OSTI ID:
6194359
Report Number(s):
CONF-8510489-
Conference Information:
Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
Country of Publication:
United States
Language:
English