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The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site."},"dataType":"OTHER COLLECTIONS","investigators":"Arthur, M.A.; Dean, W.E.","investigatorDetails":[{"firstName":"Michael","lastName":"Arthur","initials":"M.A.","orcId":"0000-0002-3028-6279"},{"firstName":"Walter","lastName":"Dean","initials":"W.E.","orcId":null}],"version":"1.0","funding":[],"studyNotes":"The SEPM volume presents the results of a coordinated, multidisciplinary study of Cretaceous carbonate and clastic rocks in cores collected along an E-W  transect across the old Cretaceous seaway that extended from the Gulf Coast to the Arctic by a team of academic, industry, and U.S. Geological Survey (USGS) scientists. The overall goal of the study was to construct a subsurface transect of mid-Cretaceous strata that were deposited in the U.S. Western Interior Seaway (WIS), ranging from pelagic, organic-carbon rich, marine hydrocarbon source rocks in Kansas and eastern Colorado to nearshore, coal-bearing units in western Colorado and Utah. This transect of cores has provided the basis for paleoenvironmental interpretation of organic-carbon burial in an epicontinental, foreland basin  setting. In part, the objectives of our study were motivated by the research emphases outlined by the Cretaceous Rhythms, Events and Resources (CRER) Project of the Global Sedimentary Geology Program. In particular, the papers in this volume focus on the Graneros Shale, Greenhorn Formation, Carlile Shale, and Niobrara Formation and equivalents in cores from drillholes from western Kansas, eastern Colorado, and eastern Utah. 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