{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "Continuity for Cretaceous Paluxy Sand in East Texas",
 "description": "<DIV STYLE=\"text-align:Left;\"><P STYLE=\"font-size:16ptmargin:7 0 7 0;\"><SPAN><SPAN>Sand-body continuity was related to the depositional systems and facies map (Caughey, 1977) and a map of the salt structures (domes, diapirs, etc.) in the East Texas Basin (Jackson and Seni, 1984) as a means to determine the continuity of the Paluxy Formation.<\/SPAN><\/SPAN><\/P><DIV><P><SPAN /><\/P><\/DIV><\/DIV>",
 "summary": "Continuity for Cretaceous Paluxy Sand in East Texas",
 "title": "Paluxy Sandstone Continuity",
 "tags": [
  "Arbuckle",
  "Oklahoma"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": "NaN",
 "maxScale": "NaN",
 "spatialReference": "",
 "accessInformation": "Caughey, C. A., 1977, Depositional systems in the Paluxy Formation (Lower Cretaceous), Northeast Texas; oil, gas, and groundwater resources: The University of Texas at Austin, Bureau of Economic Geology, Geological Circular 77-8, 59 p.\n*\nJackson, M. P. A., and Seni, S. J., 1984, Atlas of salt domes in the East Texas Basin: The University of Texas at Austin, Bureau of Economic Geology Report of Investigations No. 140, 102 p.",
 "licenseInfo": "See access and use constraints information.",
 "portalUrl": ""
}