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snippet: | Rock/Water reaction for St. Peter Sandstone |
summary: | Rock/Water reaction for St. Peter Sandstone |
accessInformation: | Odom, I. E., Doe, T. W., and Dott, R. H., Jr., 1976, Nature of feldspar-grain size relations in some quartz-rich sandstones: Journal of Sedimentary Petrology, v. 46, p. 862–870. * Odom, I. E., Willand, T. M., and Lassin, R. J., 1977, Paragenesis of authigenic minerals in St. Peter Sandstone: American Association of Petroleum Geologists Bulletin, v. 61, p. 1384–1385. |
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maxScale: | 0 |
typeKeywords: | [] |
description: | <DIV STYLE="text-align:Left;"><P STYLE="text-align:Justify;font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>The St. Peter Sandstone is a mature quartz arenite that contains little or no silt and clay, except near its perimeter. Therefore, we conclude that the potential for rock/water reaction with high CO</SPAN></SPAN><SPAN><SPAN>2</SPAN></SPAN><SPAN><SPAN> brine is low.</SPAN></SPAN></P><DIV><P><SPAN /></P></DIV></DIV> |
licenseInfo: | See access and use constraints information. |
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title: | St. Peter Rock/ Water Reaction |
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tags: | ["St. Peter Sandstone","Illinois Basin","Kentucky","Indiana"] |
culture: | en-US |
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minScale: | 0 |
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