Description: <DIV STYLE="text-align:Left;"><P STYLE="text-align:Justify;font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>Percent shale was computed from facies-distribution maps (Budnik and Smith, 1982) of the Lower and Upper Pennsylvanian-age rocks, respectively. The main assumption we made here was that the Granite Wash included only shale and coarser grained clastics but no bedded carbonates. This is, of course, not strictly true, but Dutton (1982a) did present several figures that imply relatively minor amounts of carbonate interbedded with the Granite Wash. Therefore, this map can more correctly be called "percent shale and carbonate." </SPAN></SPAN></P><DIV><DIV><P><SPAN /></P></DIV></DIV></DIV>
Service Item Id: 0cdaf7516645462e9fdf08a00e4dd5ba
Copyright Text: Dutton, S. P., 1982a, Depositional history and reservoir quality of Granite Wash, in Gustavson, T. C., Bassett, R. L., Budnik, R., Finley, R., Goldstein, A. G., McGowen, J. H., Roedder, E., Ruppel, S. C., Baumgardner, R. W., Jr., Bentley, M. E., Dutton, S. P., Fogg, G. E., Hovorka, S. D., McGookey, D. A., Ramondetta, P. J., Simpkins, W. W., Smith, D., Smith, D. A., Duncan, E. A., Griffin, J. A., Merritt, R. M., and Naiman, E. R., Geology and geohydrology of the Palo Duro Basin, Texas Panhandle: a report on the progress of the nuclear waste isolation feasibility studies, 1981: The University of Texas at Austin, Bureau of Economic Geology, Geological Circular 82-7, p. 87–90.