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...
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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
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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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