Name: woodbine_007_topsealthick_22

Display Field: source_organization

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Description: <DIV STYLE="text-align:Left;"><P STYLE="font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>The Eagle Ford shale is the low-permeability unit immediately on top of the Woodbine. A thickness map was digitized from Surles (1986) and gridded (c7woodbineg). More regional-scale stratigraphic and facies information is available from this source. The Eagle Ford has been eroded over the Sabine Uplift in the eastern part of the study area; however, the low-transmissivity Austin Chalk extends over this area.</SPAN></SPAN></P><DIV><P><SPAN /></P></DIV></DIV>

Service Item Id: 43fd3c292ed64d69a267b17bedfa7220

Copyright Text: Surles, M. A., 1986, Stratigraphy of the Eagle Ford Group (Upper Cretaceous) and its source-rock potential in the East Texas Basin: Baylor University, Master's thesis, 219 p.

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