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National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Dorcheat member
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Sandstone
    • Shale
    • Limestone
  • AAPG geologic province:
    • Arkla basin
    • East Texas basin
    • Mid-Gulf Coast basin
Publication:

Swain, F.M., 1944, Stratigraphy of Cotton Valley beds of northern Gulf Coastal Plain: American Association of Petroleum Geologists Bulletin, v. 28, no. 5, p. 577-614. [Available online, with subscription, from AAPG archives: http://www.aapg.org/datasystems or http://search.datapages.com]


Summary:

Pg. 578 (table 1), 597, 602-609. Dorcheat member, upper member of Schuler formation (redefined) of Cotton Valley group (rank raised). Defined as including the nearshore pastel, varicolored shales, and sandstones, and the equivalent offshore dark-gray fossilfierous shales, sandstone, and limestones between the base of the Hosston formation and the top of the red-green shales, sandstones (nearshore facies), and marine rocks (offshore facies) of the Shongaloo member (new). Locally, dark-gray, glauconitic, fossiliferous shale, herein named the Wesson tongue, occurs near the top of the nearshore facies of the member. Occurs between depths of 6,420 to 7,510 feet in type well. Attains its greatest thickness of 1,200 feet or more near Arkansas-Louisiana State line and on the Monroe uplift, in Morehouse Parish, Louisiana, south of which it thins gradually. In most areas, the Dorcheat is overlain with regional conformity by the Hosston formation; in central part of Monroe uplift, overlain by late Upper Cretaceous chalk; in East Texas basin, the contact is unconformable; generally the Dorcheat conformably overlies the Shongaloo; in Nevada County, Arkansas, it overlaps the Shongaloo and rests directly on the Smackover limestone; in Bowie County, Texas, it overlaps the Shongaloo and rests on Paleozoic sandstone. Age is Late Jurassic. Report includes cross sections, nomenclature chart.
Type section (subsurface; nearshore facies): depth-interval 6,420 to 7,510 ft, Atlantic Refining Company's Pinewoods Lumber Company No. 1 well, Dorcheat field discovery well, in center NE/4 NE/4 sec. 16, T. 18 S., R. 22 W., Columbia Co., AR. Named from Dorcheat oil field, Columbia Co., AR.

Source: Publication; US geologic names lexicon (USGS Bull. 1200, p. 1141); supplemental information from GNU records (USGS DDS-6; Denver GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Dorcheat Member
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Arkla basin
Publication:

Mann, C.J., and Thomas, W.A., 1964, Cotton Valley Group (Jurassic) nomenclature, Louisiana and Arkansas: Gulf Coast Association of Geological Societies Transactions, v. 14, p. 143-152.


Summary:

Restricted to the nearshore facies of the Upper Jurassic Schuler Formation of the Cotton Valley Group of Swain (1944) in AR and northern LA. Composed of pastel, varicolored shale and sandstone. Cross sections. Equivalent to the Hico Shale and Knowles Limestone (both new) basinward. Extends in southern AR almost to the AR-LA border in the Arkla basin. Overlies Shongaloo Member ("restricted") of Schuler. Underlies Hosston Formation. Is equivalent to parts of the Hico Shale and Terryville Sandstone (both newly named) of the Cotton Valley downdip in LA.

Source: GNU records (USGS DDS-6; Denver GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

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