Zobrazeno 1 - 9
of 9
pro vyhledávání: '"A. E. Weidie"'
Autor:
Donald E. Burch, A. E. Weidie
Publikováno v:
AAPG Bulletin. 78
In southwestern Choctaw County, Alabama, the Eagle Mills Formation consists of alluvial-fan red beds deposited in a Mesozoic graben. The Exxon No. 1 Smith Lumber Co. well penetrated the upper 2,210 ft of the Eagle Mills, and it is divided into eight
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6af98eed667e8d4a4845f30d59f6f04b
https://doi.org/10.1306/a25fed65-171b-11d7-8645000102c1865d
https://doi.org/10.1306/a25fed65-171b-11d7-8645000102c1865d
Publikováno v:
Water Resources Research. 15:1521-1535
Xel Ha is a lagoon whose location and morphology are partly controlled by the fracture pattern in upper Pleistocene coral reef limestone. Chemical, isotopic, and hydrologic observations were made nearby where groundwater could be sampled. In addition
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1114534fcfe5e4c4262c03c9ea43e1da
https://doi.org/10.1029/wr015i006p01521
https://doi.org/10.1029/wr015i006p01521
Publikováno v:
AAPG Bulletin. 46
The Difunta Group of the Parras Basin, southern Coahuila and western Nuevo Leon, Mexico, consists of two major intertonguing lithic facies with a composite thickness of approximately 4,000 meters. Three gray, brown, red, and green, partly variegated,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f6d42a036e643761d3ed458e42328d2
https://doi.org/10.1306/bc743829-16be-11d7-8645000102c1865d
https://doi.org/10.1306/bc743829-16be-11d7-8645000102c1865d
Autor:
Grover E. Murray, A. E. Weidie
Publikováno v:
AAPG Bulletin. 51
The Parras basin, in southern Coahuila and western Nuevo Leon, Mexico, contains 4,500-6,000 meters of Upper Cretaceous and lower Tertiary terrigenous sedimentary rocks. Approximately 1,500-2,100 meters of Lower Cretaceous carbonate rocks and 2,000-3,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1bde439c3cf38cee7f2f1138fdd53b76
https://doi.org/10.1306/5d25c0c1-16c1-11d7-8645000102c1865d
https://doi.org/10.1306/5d25c0c1-16c1-11d7-8645000102c1865d
Autor:
Joseph D. Martinez, A. E. Weidie
Publikováno v:
AAPG Bulletin. 54
Several authors have reported intrusive gypsum in northeastern Mexico. Salt diapirism also has been inferred. Recent evidence from cores indicates that the complete sequence of evaporites behaved as a mobile unit in response to tight folding. The "Mi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::949fefc4d0fa594787a62aa39964e82f
https://doi.org/10.1306/5d25ca23-16c1-11d7-8645000102c1865d
https://doi.org/10.1306/5d25ca23-16c1-11d7-8645000102c1865d
Publikováno v:
AAPG Bulletin. 56
The Parras and Sabinas basins in Coahuila and Nuevo Leon and the Ojinaga basin in northeastern Chihuahua were the principal sites of Late Cretaceous sedimentation in northeastern Mexico. Comparative study of these basins provides insight into the Lat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4fc8f9be5df32386e97ee1afec09f9b3
https://doi.org/10.1306/819a4180-16c5-11d7-8645000102c1865d
https://doi.org/10.1306/819a4180-16c5-11d7-8645000102c1865d
Autor:
J. A. Wolleben, A. E. Weidie
Publikováno v:
AAPG Bulletin. 53
Ammonites have been found in the basal La Casita Formation (= Cotton Valley of U. S.) near its contact with the Zuloaga Limestone (= Smackover Limestone of U. S.) near Monterrey, Mexico. An early Kimeridgian age is indicated for the basal La Casita.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a8d0406c0fdd9b5dd5cde859e583aa4
https://doi.org/10.1306/5d25c963-16c1-11d7-8645000102c1865d
https://doi.org/10.1306/5d25c963-16c1-11d7-8645000102c1865d
Publikováno v:
Geological Society of America Bulletin. 85:1603
The Parras and La Popa basins of Coahuila and Nuevo Leon, Mexico, have a composite thickness of about 5.4 km of paralic sedimentary rock (Parras Formation and Difunta Group) deposited during Late Cretaceous to Paleocene time. Detritus of sedimentary,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0cbac920e8c3925097b5007fddbb0ba
https://doi.org/10.1130/0016-7606(1974)85<1603:sasotp>2.0.co
https://doi.org/10.1130/0016-7606(1974)85<1603:sasotp>2.0.co