Regional structural cross-sections, Mid-Permian to Quaternary strata, Texas Panhandle and eastern New Mexico; Mapping of Quaternary of Rolling Plains

dc.contributorUniversity of Texas at Austin. Bureau of Economic Geology
dc.contributorGustavson, Thomas C.
dc.contributorBaumgardner, Robert W.
dc.contributorCaran, S. Christopher
dc.contributorHoadley, Ann D.
dc.coverage.box-105,-100,36.75,33.75
dc.coverage.scale247500
dc.coverage.scale506880
dc.coverage.spatialNew Mexico
dc.creatorMcGookey, Douglas A.
dc.date.accessioned2019-10-28T15:51:31Z
dc.date.available2019-10-28T15:51:31Z
dc.date.issued1988
dc.descriptionTo obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: CS0008.
dc.description.abstractThe Palo Duro Basin of the Texas Panhandle and eastern New Mexico contains bedded Permian salts of sufficient thickness and depth for the basin to be considered as a potential site for long-term storage and isolation of high-level nuclear waste. Salt (primarily halite) is a desirable host rock because of its low permeability, high thermal conductivity, low moisture content, and high gamma-ray shielding properties (Johnson, 1976b). A major concern that was addressed during the waste isolation study of the Texas Panhandle region is the long-term integrity of the bedded-salt host rock. Areas where salt has been removed by dissolution have been identified beneath the Southern High Plains, along the eastern and western escarpments of the Southern High Plains, and along the Canadian River valley (Gustavson and others, 1980b; Presley, 1980a, 1980b; Gustavson and Finley, 1985; Gustavson, 1986). Regional cross sections of mid-Permian to Quaternary strata in the Texas Panhandle and east- ern New Mexico illustrate lithologic and structural relations that are interpreted to have resulted from the regional dissolution of salt and the collapse of overlying strata. The cross sections were constructed using gamma-ray logs, sample logs, and surface geologic maps (Handford, 1980a; McGillis, 1980). Gamma-ray logs are shown on the cross sections because they best demonstrate variations in evap- orite strata. Figure 1 is an index map depicting the locations of the cross sections. Stratigraphic nomen- clature used on the cross sections is given in table 1.
dc.description.departmentUT Libraries
dc.description.departmentBureau of Economic Geology
dc.format.dimensions15 maps ; 39 x 77 cm. or smaller folded to 28 x 23 cm. or smaller in envelope 30 x 24 cm.
dc.identifierCS0008
dc.identifier.urihttps://hdl.handle.net/2152/77730
dc.identifier.urihttp://dx.doi.org/10.26153/tsw/4819
dc.publisherUniversity of Texas at Austin. Bureau of Economic Geology
dc.relation.ispartofVirtual Landscapes of Texas
dc.relation.ispartofCross Sections
dc.relation.ispartofseriesCross Sections (University of Texas at Austin. Bureau of Economic Geology), no. 8
dc.rights.restrictionOpen
dc.subjectGeology, Stratigraphic -- Permian -- Maps
dc.subjectGeology, Stratigraphic -- Quaternary -- Maps
dc.subjectGeology, Structural -- Maps
dc.subjectSalt deposits -- New Mexico -- Maps
dc.subjectSalt deposits -- Texas -- Texas Panhandle -- Maps
dc.titleRegional structural cross-sections, Mid-Permian to Quaternary strata, Texas Panhandle and eastern New Mexico; Mapping of Quaternary of Rolling Plains
dc.title.alternativeMapping of Quaternary of Rolling Plains
dc.typeOther

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