{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "Rock/Water reaction for St. Peter Sandstone",
 "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>",
 "summary": "Rock/Water reaction for St. Peter Sandstone",
 "title": "St. Peter Rock/ Water Reaction",
 "tags": [
  "St. Peter Sandstone",
  "Illinois Basin",
  "Kentucky",
  "Indiana"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": "NaN",
 "maxScale": "NaN",
 "spatialReference": "",
 "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\u2013870.\n*\nOdom, 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\u20131385.",
 "licenseInfo": "See access and use constraints information.",
 "portalUrl": ""
}