Intertongued Dakota Sandstone-Mancos Shale members of surface and subsurface in San Juan basin, New Mexico and Colorado
Three wedges of transgressive marine Mancos Shale, deposited offshore, intertongue with four Dakota Sandstone units, largely shoreface deposits. Contacts between shoreface and offshore lithologies trend approximately north-south, with nonmarine Dakota main body sandstones to the west. Submarine bar sandstones trending northwest-southeast are locally developed near the shoreface-offshore transition. This succession was deposited during approximately 4 m.y. of the transgressive phase of the Greenhorn cyclothem. Each Dakota-Mancos sandstone-shale pair may represent (1) a fourth-order eustatic cycle or (2) regional tectonic and local sedimentologic overprints of two third-order Vail cycles. Detailed analyses of trace elements within shales and primary sedimentary structures and trace fossils of sandstones, combined with geophysical logs and regional paleontologic control, were invaluable in this first, basin-wide, surface and subsurface paleoenvironmental study of these complex strata.
- OSTI ID:
- 5923696
- Report Number(s):
- CONF-880301-
- Resource Relation:
- Conference: Annual meeting of the American Association of Petroleum Geologists, Houston, TX, USA, 20-23 Mar 1988
- Country of Publication:
- United States
- Language:
- English
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COLORADO
PETROLEUM DEPOSITS
NEW MEXICO
SEDIMENTARY BASINS
GEOPHYSICAL SURVEYS
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PALEONTOLOGY
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