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...
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| Format: | eBook |
| Language: | English |
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Berlin, Heidelberg :
Springer Berlin Heidelberg : Imprint : Springer,
2002.
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| Online Access: | Connect to the full text of this electronic book |
| Summary: | 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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| Item Description: | Electronic resource. |
| Physical Description: | 1 online resource (XII, 324 pages 112 illustrations) |
| ISBN: | 9783642563966 (electronic bk.) 3642563961 (electronic bk.) |