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= Assessment of continuous oil resources in the Eastern Great Basin Province of Nevada, Utah, and Idaho, 2018 =
{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Assessment of continuous oil resources in the Eastern Great Basin Province of Nevada, Utah, and Idaho, 2018", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "fs20193002", "url": "https://pubs.usgs.gov/publication/fs20193002"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70204134}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/fs20193002", "url": "https://doi.org/10.3133/fs20193002"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Fact Sheet"}], "datePublished": "2019", "dateModified": "2019-07-16", "abstract": "The U.S. Geological Survey (USGS) quantitatively assessed the\u00a0potential for undiscovered, technically recoverable continuous oil and gas\u00a0resources in the Eastern Great Basin Province (Anna and others, 2007) of\u00a0Nevada, Utah, and Idaho (fig. 1). The assessment focused on the area of\u00a0the province between the Roberts Mountains and Sevier thrust systems\u00a0(Peterson, 1994). The major petroleum source rocks within this area are the\u00a0Upper Devonian\u2013Lower Mississippian Pilot Shale and the Mississippian\u00a0Chainman Formation (Gutschick and Rodriquez, 1979; Poole and Claypool,\u00a01984; Giles, 1994; Trexler and others, 1995). The geologic model applied\u00a0to the Pilot Shale and shales in the Chainman Formation is for these shales\u00a0to have achieved generative maturity for oil by burial to at least 8,700 feet\u00a0(2,652 meters) within some of the Neogene extensional basins (Grabb, 1994;\u00a0Anna and others, 2007). 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The U.S. Geological Survey (USGS) quantitatively assessed the potential for undiscovered, technically recoverable continuous oil and gas resources in the Eastern Great Basin Province (Anna and others, 2007) of Nevada, Utah, and Idaho (fig. 1). The assessment focused on the area of the province between the Roberts Mountains and Sevier thrust systems (Peterson, 1994). The major petroleum source rocks within this area are the Upper Devonian–Lower Mississippian Pilot Shale and the Mississippian Chainman Formation (Gutschick and Rodriquez, 1979; Poole and Claypool, 1984; Giles, 1994; Trexler and others, 1995). The geologic model applied to the Pilot Shale and shales in the Chainman Formation is for these shales to have achieved generative maturity for oil by burial to at least 8,700 feet (2,652 meters) within some of the Neogene extensional basins (Grabb, 1994; Anna and others, 2007). Areas that satisfy this depth requirement were defined using modeled gravity data that were calibrated to the petroleum system in Railroad Valley and Pine Valley in Nevada (Barker and Peterson, 1991; Ïnan and Davis, 1994; Meissner, 1995; Anna and others, 2007). 
 
== Table of Contents ==
* Introduction
* Total Petroleum Systems and Assessment Units
* Undiscovered Resources Summary
* References Cited