Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Jon T. Ehrhart"'
Publikováno v:
International Journal of Speleology, Vol 46, Iss 2, Pp 169-180 (2017)
Evaporite karst throughout the Gypsum Plain of west Texas is complex and extensive, including manifestations ranging from intrastratal brecciation and hypogene caves to epigene features and suffosion caves. Recent advances in hydrocarbon exploration
Externí odkaz:
https://doaj.org/article/ef313f376305458ab15d19e6f54ed836
Publikováno v:
International Journal of Speleology, Vol 47, Iss 3, Pp 293-305 (2018)
Diverse karst phenomena occur throughout the Gypsum Plain where the Castile Formation crops out over ~1800 km2 in West Texas and southeastern New Mexico. Hypergene karst is extensive and widespread, while traditional hypogene karst manifestations (bo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ff568c03d0e9ef2c12393071841c9c90
https://scholarcommons.usf.edu/ijs/vol47/iss3/3/
https://scholarcommons.usf.edu/ijs/vol47/iss3/3/
Publikováno v:
Journal of Environmental and Engineering Geophysics. 22:411-420
The Delaware Basin of W Texas and SE New Mexico is the western subdivision of the Permian Basin and a northern extension of the Chihuahuan Desert. The major evaporite unit within the Delaware Basin is the Castile Formation, which consists of gypsum/a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f573e84c2343e13e33a69ab06dbb584e
https://doi.org/10.2113/jeeg22.4.411
https://doi.org/10.2113/jeeg22.4.411
Publikováno v:
International Journal of Speleology, Vol 46, Iss 2, Pp 169-180 (2017)
Evaporite karst throughout the Gypsum Plain of west Texas is complex and extensive, including manifestations ranging from intrastratal brecciation and hypogene caves to epigene features and suffosion caves. Recent advances in hydrocarbon exploration
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::074a08624b5ebae99cec22c7fdf0d94b
http://scholarcommons.usf.edu/ijs/vol46/iss2/4/
http://scholarcommons.usf.edu/ijs/vol46/iss2/4/