Soft Plate and Impact Tectonics:
The rigid plate kinematics theory explains most of the current geodetic, geophysical and tectonic data on earth but fails to account for some anomalies. Spatial geodetic data has shown that oceanic plate interiors are not rigid because incipient boudinage and homogeneous shortening develop before bu...
Gespeichert in:
| 1. Verfasser: | |
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
2002
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| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | The rigid plate kinematics theory explains most of the current geodetic, geophysical and tectonic data on earth but fails to account for some anomalies. Spatial geodetic data has shown that oceanic plate interiors are not rigid because incipient boudinage and homogeneous shortening develop before buckling of the entire lithosphere. Seismicity and faulting show that the oceanic lithosphere can deform at strain rates above stable continental interiors but below plate boundary zones of variable widths. This is due to the weakening effects of fluids during hydrothermal sea floor metamorphism commonly found in oceans. Furthermore, the test of finiate strain and the implications of the Wilson Cycle are discussed. The Earth is a dissipative dynamical system open to external forcing |
| Beschreibung: | 1 Online-Ressource (XII, 324 p) |
| ISBN: | 9783642563966 |
| DOI: | 10.1007/978-3-642-56396-6 |
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| 520 | |a The rigid plate kinematics theory explains most of the current geodetic, geophysical and tectonic data on earth but fails to account for some anomalies. Spatial geodetic data has shown that oceanic plate interiors are not rigid because incipient boudinage and homogeneous shortening develop before buckling of the entire lithosphere. Seismicity and faulting show that the oceanic lithosphere can deform at strain rates above stable continental interiors but below plate boundary zones of variable widths. This is due to the weakening effects of fluids during hydrothermal sea floor metamorphism commonly found in oceans. Furthermore, the test of finiate strain and the implications of the Wilson Cycle are discussed. The Earth is a dissipative dynamical system open to external forcing | ||
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| dewey-ones | 551 - Geology, hydrology, meteorology |
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| discipline | Geologie / Paläontologie |
| doi_str_mv | 10.1007/978-3-642-56396-6 |
| format | Electronic eBook |
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| id | DE-604.BV045177197 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:46Z |
| institution | BVB |
| isbn | 9783642563966 |
| language | English |
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| spelling | Ribeiro, Antnio Verfasser aut Soft Plate and Impact Tectonics by Antnio Ribeiro Berlin, Heidelberg Springer Berlin Heidelberg 2002 1 Online-Ressource (XII, 324 p) txt rdacontent c rdamedia cr rdacarrier The rigid plate kinematics theory explains most of the current geodetic, geophysical and tectonic data on earth but fails to account for some anomalies. Spatial geodetic data has shown that oceanic plate interiors are not rigid because incipient boudinage and homogeneous shortening develop before buckling of the entire lithosphere. Seismicity and faulting show that the oceanic lithosphere can deform at strain rates above stable continental interiors but below plate boundary zones of variable widths. This is due to the weakening effects of fluids during hydrothermal sea floor metamorphism commonly found in oceans. Furthermore, the test of finiate strain and the implications of the Wilson Cycle are discussed. The Earth is a dissipative dynamical system open to external forcing Earth Sciences Geology Geophysics/Geodesy Oceanography Earth sciences Geophysics Plattentektonik (DE-588)4046317-5 gnd rswk-swf Plattentektonik (DE-588)4046317-5 s 1\p DE-604 Erscheint auch als Druck-Ausgabe 9783642632358 https://doi.org/10.1007/978-3-642-56396-6 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Ribeiro, Antnio Soft Plate and Impact Tectonics Earth Sciences Geology Geophysics/Geodesy Oceanography Earth sciences Geophysics Plattentektonik (DE-588)4046317-5 gnd |
| subject_GND | (DE-588)4046317-5 |
| title | Soft Plate and Impact Tectonics |
| title_auth | Soft Plate and Impact Tectonics |
| title_exact_search | Soft Plate and Impact Tectonics |
| title_full | Soft Plate and Impact Tectonics by Antnio Ribeiro |
| title_fullStr | Soft Plate and Impact Tectonics by Antnio Ribeiro |
| title_full_unstemmed | Soft Plate and Impact Tectonics by Antnio Ribeiro |
| title_short | Soft Plate and Impact Tectonics |
| title_sort | soft plate and impact tectonics |
| topic | Earth Sciences Geology Geophysics/Geodesy Oceanography Earth sciences Geophysics Plattentektonik (DE-588)4046317-5 gnd |
| topic_facet | Earth Sciences Geology Geophysics/Geodesy Oceanography Earth sciences Geophysics Plattentektonik |
| url | https://doi.org/10.1007/978-3-642-56396-6 |
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