The Permian of Northern Pangea: Volume 2: Sedimentary Basins and Economic Resources
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...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1995
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| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | 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. These two volumes attempt to bring together some of the widely scattered observations about these fascinating rocks, at least for the northern (predominantly nonglacial) parts of Pangea |
| Beschreibung: | 1 Online-Ressource (VII, 312 p) |
| ISBN: | 9783642785900 |
| DOI: | 10.1007/978-3-642-78590-0 |
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| 520 | |a 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. These two volumes attempt to bring together some of the widely scattered observations about these fascinating rocks, at least for the northern (predominantly nonglacial) parts of Pangea | ||
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Datensatz im Suchindex
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| dewey-full | 551 |
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| dewey-ones | 551 - Geology, hydrology, meteorology |
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| dewey-search | 551 |
| dewey-sort | 3551 |
| dewey-tens | 550 - Earth sciences |
| discipline | Geologie / Paläontologie |
| doi_str_mv | 10.1007/978-3-642-78590-0 |
| format | Electronic eBook |
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| id | DE-604.BV045178354 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:49Z |
| institution | BVB |
| isbn | 9783642785900 |
| language | English |
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| physical | 1 Online-Ressource (VII, 312 p) |
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| spelling | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources edited by Peter A. Scholle, Tadeusz M. Peryt, Dana S. Ulmer-Scholle Berlin, Heidelberg Springer Berlin Heidelberg 1995 1 Online-Ressource (VII, 312 p) txt rdacontent c rdamedia cr rdacarrier 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. These two volumes attempt to bring together some of the widely scattered observations about these fascinating rocks, at least for the northern (predominantly nonglacial) parts of Pangea Earth Sciences Geology Sedimentology Earth sciences Scholle, Peter A. edt Peryt, Tadeusz M. edt Ulmer-Scholle, Dana S. edt Erscheint auch als Druck-Ausgabe 9783642785924 https://doi.org/10.1007/978-3-642-78590-0 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources Earth Sciences Geology Sedimentology Earth sciences |
| title | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources |
| title_auth | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources |
| title_exact_search | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources |
| title_full | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources edited by Peter A. Scholle, Tadeusz M. Peryt, Dana S. Ulmer-Scholle |
| title_fullStr | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources edited by Peter A. Scholle, Tadeusz M. Peryt, Dana S. Ulmer-Scholle |
| title_full_unstemmed | The Permian of Northern Pangea Volume 2: Sedimentary Basins and Economic Resources edited by Peter A. Scholle, Tadeusz M. Peryt, Dana S. Ulmer-Scholle |
| title_short | The Permian of Northern Pangea |
| title_sort | the permian of northern pangea volume 2 sedimentary basins and economic resources |
| title_sub | Volume 2: Sedimentary Basins and Economic Resources |
| topic | Earth Sciences Geology Sedimentology Earth sciences |
| topic_facet | Earth Sciences Geology Sedimentology Earth sciences |
| url | https://doi.org/10.1007/978-3-642-78590-0 |
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