{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "Percent Evaporates for Cedar Keys Lawson",
 "description": "<DIV STYLE=\"text-align:Left;\"><P STYLE=\"font-size:16ptmargin:7 0 7 0;\"><SPAN><SPAN>To characterize the continuity of the top seal, we chose the map of Chen (1965), which shows the percent evaporites in the Paleocene Cedar Keys Dolomite<\/SPAN><\/SPAN><\/P><DIV><P><SPAN /><\/P><\/DIV><\/DIV>",
 "summary": "Percent Evaporates for Cedar Keys Lawson",
 "title": "Percent Evaporates for Cedar / Keys (Continuity of Top Seal)",
 "tags": [
  "Central Florida",
  "Cedar Keys/ Lawson"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": 0,
 "maxScale": 0,
 "spatialReference": "",
 "accessInformation": "Chen, S. C., 1965, The regional stratigraphic analysis of Paleocene and Eocene rocks of Florida: Florida Geological Survey Bulletin No. 45, 105 p.",
 "licenseInfo": "See access and use constraints information."
}