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dc.creatorOrr, S. R.en_US
dc.creatorFaure, Gunteren_US
dc.creatorBotoman, Georgeen_US
dc.date.accessioned2006-07-07T01:59:19Z
dc.date.available2006-07-07T01:59:19Z
dc.date.issued1982-03en_US
dc.identifier.citationThe Ohio Journal of Science. v82, n1 (March, 1982), 52-54en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/22831
dc.descriptionAuthor Institution: Department of Geology and Mineralogy, Ohio State University ; Division of Geological Survey, Ohio Department of Natural Resources, Fountain Squareen_US
dc.description.abstractA carbonate concretion from the shale bed overlying the No. 5 coal of Pennsylvanian age in Tuscarawas County is composed of siderite and contains pyrite, barite, sphalerite and traces of calcite in its interior and in fractures. The siderite has 8I 3C= +0.65%o, Sr=289 ppm and 87Sr/86Sr=0.7110±0.0009- These results indicate that the siderite was deposited from brackish water in the pore spaces of the sediment and discredit the hypothesis that the carbonate ions originated by oxidation of peat or organic material. The barite has 8 S=— 4.6%o, indicating that it was not precipitated from sea water. Pyrite and sphalerite have 8 S= — 10.8%o and — 4.6%o, respectively, and were not deposited in isotopic equilibrium with each other. The sulfur in all three minerals is enriched in l6S as a result of bacterial reduction of sulfate to sulfide.en_US
dc.format.extent290160 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleIsotopic Study of Siderite Concretion, Tuscarawas County, Ohioen_US


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