A sulfate conundrum; dissolved sulfates of deep saline brines and carbonate-associated sulfates

Sulfates in deeply circulating brines and carbonate-associated sulfates (CAS) within sedimentary units of the Cambrian strata in the Illinois Basin record a complex history. Dissolved sulfate within the Mt. Simon Sandstone brines exhibits average δ34SSO4 values of 35... Full description

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doi: 10.1016/j.gca.2016.06.033
Authors:Labotka, D.M.; Panno, S.V.; Locke, R.A.
Volume Title:Geochimica et Cosmochimica Acta
Source:Geochimica et Cosmochimica Acta, Vol.190, p.53-71. Publisher: Elsevier, New York, NY, International. ISSN: 0016-7037
Publication Date:2016
Note:In English. 119 refs.; illus., incl. 2 tables, sketch map
Subjects:Basement; Basin analysis; Bonneterre Formation; Brines; Cambrian; Carbonates; Chemically precipitated rocks; Crystal chemistry; Eau Claire Formation; Evaporites; Fluid phase; Galesville Sandstone; Isotope ratios; Isotopes; Lithostratigraphy; Marine sediments; Metal ores; Metallogeny; Meteoric water; Mineral deposits, genesis; Mineral exploration; Mississippi valley-type deposits; Mount Simon Sandstone; O-18/O-16; Oxygen; Paleozoic; Permian; S-34/S-32; Saline composition; Sedimentary rocks; Sediments; Solutes; Stable isotopes; Sulfates; Sulfur; Upper Cambrian; Water-rock interaction; Illinois; Illinois Basin; Michigan Basin; Missouri; North America; United States; Viburnum Trend; Ironton Formation
Coordinates:N373000 N393000 W0880000 W0930000
Record ID:2016094229
Copyright Information:GeoRef, Copyright 2020 American Geosciences Institute. Reference includes data from CAPCAS, Elsevier Scientific Publishers, Amsterdam, Netherlands
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