{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "Fault locations for St. Peter Sandstone",
 "description": "<DIV STYLE=\"text-align:Left;\"><P STYLE=\"font-size:16ptmargin:7 0 7 0;\"><SPAN><SPAN>Several authors indicated that the sands within the St. Peter Sandstone are continuous, especially in the middle portions of the unit (Kreutzfeld, 1982; Barnes and others, 1992). The St. Peter Sandstone is partially offset by a number of faults, and these faults can significantly affect sand-body continuity. Therefore, we chose to use the map of Collinson and others (1988), which shows the locations of major faults that offset the St. Peter Sandstone to characterize sand-body continuity, because faulting rather than lithology is the principal factor influencing sand-body continuity of the St. Peter in the central Illinois Basin.<\/SPAN><\/SPAN><\/P><DIV><DIV><P><SPAN /><\/P><\/DIV><\/DIV><\/DIV>",
 "summary": "Fault locations for St. Peter Sandstone",
 "title": "St. Peter Faults",
 "tags": [
  "St. Peter Sandstone",
  "Illinois Basin",
  "Kentucky",
  "Indiana"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": 0,
 "maxScale": 0,
 "spatialReference": "",
 "accessInformation": "Collinson, C., Sargent, M. L., and Jennings, J. R., 1988, Chapter 14: Illinois Basin region, in Sloss, L. L., ed., The Geology of North America, v. D-2, Sedimentary Cover\u2014North American Craton: U.S.: Decade of North American Geology: Geological Society of America, p. 383\u2013426.",
 "licenseInfo": "See access and use constraints information."
}