Fluid inclusion chemistry in the exploration for Mississippi Valley-type deposits: an example from East Tennessee, U.S.A.
dc.contributor.author | Haynes, Frederick M. | en_US |
dc.contributor.author | Kesler, Stephen E. | en_US |
dc.date.accessioned | 2006-04-07T19:53:50Z | |
dc.date.available | 2006-04-07T19:53:50Z | |
dc.date.issued | 1987 | en_US |
dc.identifier.citation | Haynes, Frederick M., Kesler, Stephen E. (1987)."Fluid inclusion chemistry in the exploration for Mississippi Valley-type deposits: an example from East Tennessee, U.S.A.." Applied Geochemistry 2(3): 321-327. <http://hdl.handle.net/2027.42/26717> | en_US |
dc.identifier.uri | http://www.sciencedirect.com/science/article/B6VDG-4893PCC-6/2/a4d45b8e9e910eb4e371d6f53e44e392 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/26717 | |
dc.description.abstract | Scanning electron microscopy and energy dispersive analysis of fluid inclusion decrepitates in sparry dolomite cements associated with sphalerite mineralization in the Mascot-Jefferson City Mississippi Valley-type district of East Tennessee show a markedly lower Na/Ca ratio than those in dolomites unassociated with ore. The exploration potential of this variation in fluid inclusion chemistry has been evaluated by analyzing inclusion decrepitates from white sparry dolomite along a 150 m traverse in the New Market West mine area. The traverse extends from the central portion of a large domal collapsebreccia orebody with greater than 3% Zn, into the dolomite-veined, but unmineralized Knox Group limestones. Ratios of Na/Ca as low as 0.8-1.2 were common in dolomite-hosted decrepitates from the high-grade collapse ores. This anomalous decrepitate chemistry was not observed in sparry dolomites less than 12 m from the margins of the breccia bodies where Na/Ca ratios ranged from 1.8 to 3.6. Dolomite cements in low grade (<1.0% Zn) parts of the collapse bodies showed the greatest variation in Na/Ca ratio, with values ranging from 0.9 to 3.5. No systematic trends were observed in K/Na and S/Cl ratios from the same samples. | en_US |
dc.format.extent | 544343 bytes | |
dc.format.extent | 3118 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Elsevier | en_US |
dc.title | Fluid inclusion chemistry in the exploration for Mississippi Valley-type deposits: an example from East Tennessee, U.S.A. | en_US |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | en_US |
dc.subject.hlbsecondlevel | Geology and Earth Sciences | en_US |
dc.subject.hlbsecondlevel | Chemistry | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1063, U.S.A. | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1063, U.S.A. | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/26717/1/0000267.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1016/0883-2927(87)90047-3 | en_US |
dc.identifier.source | Applied Geochemistry | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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