Author: Spencer G. Lucas
Publisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Science
Languages : en
Pages : 52
Book Description
Traces of a Permian Seacoast
The Carboniferous-Permian Transition
Author: Spencer G. Lucas
Publisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 481
Book Description
Publisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 481
Book Description
The Nonmarine Permian
Author: Spencer G. Lucas
Publisher: New Mexico Museum of Natural History and Science
ISBN:
Category :
Languages : en
Pages : 371
Book Description
Publisher: New Mexico Museum of Natural History and Science
ISBN:
Category :
Languages : en
Pages : 371
Book Description
American Permian Vertebrates
Author: Samuel Wendell Williston
Publisher:
ISBN:
Category : Paleontology
Languages : en
Pages : 724
Book Description
Publisher:
ISBN:
Category : Paleontology
Languages : en
Pages : 724
Book Description
Permian Field Conference to the Guadalupe Mountains
Author: Philip Burke King
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 71
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 71
Book Description
Mid-Permian Phosphoria Sea in Nevada and the Upwelling Model
Author: Keith Brindley Ketner
Publisher:
ISBN:
Category : Formations (Geology)
Languages : en
Pages : 32
Book Description
Publisher:
ISBN:
Category : Formations (Geology)
Languages : en
Pages : 32
Book Description
The Permian Extinction and the Tethys
Author: A. M. Celâl ?engör
Publisher: Geological Society of America
ISBN: 0813724481
Category : Science
Languages : en
Pages : 110
Book Description
The extinction that wiped out 95% of the living species at the end of the Paleozoic era can be explained by the fact that when it happened, all landmasses were one continent, Pangea, with an inner ocean, the Paleo-Tethys. This ocean included the richest n
Publisher: Geological Society of America
ISBN: 0813724481
Category : Science
Languages : en
Pages : 110
Book Description
The extinction that wiped out 95% of the living species at the end of the Paleozoic era can be explained by the fact that when it happened, all landmasses were one continent, Pangea, with an inner ocean, the Paleo-Tethys. This ocean included the richest n
Triassic Hall
Author: Jaenet Guggenheim
Publisher: New Mexico Museum of Natural History and Science
ISBN:
Category :
Languages : en
Pages : 142
Book Description
Publisher: New Mexico Museum of Natural History and Science
ISBN:
Category :
Languages : en
Pages : 142
Book Description
The Permian Reef Complex of the Guadalupe Mountains Region, Texas and New Mexico
Author: Norman Dennis Newell
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 336
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 336
Book Description
The Permian of Northern Pangea
Author: Peter A. Scholle
Publisher: Springer Science & Business Media
ISBN: 364278593X
Category : Science
Languages : en
Pages : 263
Book Description
The Permian was a remarkable time period. It represents the maximum stage of Pangean continental assembly, includes a major global climatic shift from glacial to nonglacial conditions (icehouse-greenhouse transition), and is ter minated by one of the most profound faunal/floral extinction events in the Earth's history. In addition, Permian oceans, although poorly understood, must have had some quite unique characteristics. Permian seas reached the most extreme values of carbon, sulfur, and strontium isotopic ratios ever achieved in Phanerozoic time, and the isotopic ratios of all three elements abruptly returned to more "normal" values at, or very close to, the Permo Triassic boundary. Finally, the Permian is marked by an abundance of important sedimentary mineral resources. It has large fossil fuel concentra tions (coal, oil, and natural gas), enormous phosphate reserves, and very extensive evaporite deposits, including gypsum, anhydrite, and halite, as well as a variety of potash salts. Study of the Permian has been hampered, however, by a number of factors. These include a scattered geologic literature (presented in a variety of languages), a confusing regional and global stratigraphic framework (based, in part, on inadequate type sections), and largely provincial, often poorly correlatable faunas. All have contributed to the sparsity and inadequacy of overviews of this critical geological interval. The two volumes attempts to bring together some of the widely scattered observations about these fascinating rocks, at least for the northern (pre dominantly nonglacial) parts of Pangea.
Publisher: Springer Science & Business Media
ISBN: 364278593X
Category : Science
Languages : en
Pages : 263
Book Description
The Permian was a remarkable time period. It represents the maximum stage of Pangean continental assembly, includes a major global climatic shift from glacial to nonglacial conditions (icehouse-greenhouse transition), and is ter minated by one of the most profound faunal/floral extinction events in the Earth's history. In addition, Permian oceans, although poorly understood, must have had some quite unique characteristics. Permian seas reached the most extreme values of carbon, sulfur, and strontium isotopic ratios ever achieved in Phanerozoic time, and the isotopic ratios of all three elements abruptly returned to more "normal" values at, or very close to, the Permo Triassic boundary. Finally, the Permian is marked by an abundance of important sedimentary mineral resources. It has large fossil fuel concentra tions (coal, oil, and natural gas), enormous phosphate reserves, and very extensive evaporite deposits, including gypsum, anhydrite, and halite, as well as a variety of potash salts. Study of the Permian has been hampered, however, by a number of factors. These include a scattered geologic literature (presented in a variety of languages), a confusing regional and global stratigraphic framework (based, in part, on inadequate type sections), and largely provincial, often poorly correlatable faunas. All have contributed to the sparsity and inadequacy of overviews of this critical geological interval. The two volumes attempts to bring together some of the widely scattered observations about these fascinating rocks, at least for the northern (pre dominantly nonglacial) parts of Pangea.