Difference between revisions of "The Global Paleogeographical Reconstruction of the Triassic and the Paleoposiont of India"
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==Abstract== | ==Abstract== | ||
− | Following the production of a series of three paleogeographical reconstructions for the Paleocene, Cretaceous and Jurassic, a further reconstruction has been made here for the Triassic period, with the assistance of paleomagnetic data. The data provided by mutual fragment positions and paleomagnetic vectors, are best reconciled if the data is treated in an expanding Earth framework, and gives credence to the view that this represents the real evolution of the Earth. In particular a new solution of the case of Indian paleoposition is given which could constitute the key to the reinterpretation of the Eurasia paleogeography throughout geological time. | + | Following the production of a series of three paleogeographical reconstructions for the Paleocene, Cretaceous and Jurassic, a further reconstruction has been made here for the Triassic period, with the assistance of paleomagnetic data. The data provided by mutual fragment positions and paleomagnetic vectors, are best reconciled if the data is treated in an expanding Earth framework, and gives credence to the view that this represents the real evolution of the Earth. In particular a new solution of the case of Indian paleoposition is given which could constitute the key to the reinterpretation of the Eurasia paleogeography throughout geological time. |
− | [[Category:Cosmology]] | + | [[Category:Scientific Paper|global paleogeographical reconstruction triassic paleoposiont india]] |
+ | |||
+ | [[Category:Cosmology|global paleogeographical reconstruction triassic paleoposiont india]] |
Latest revision as of 20:02, 1 January 2017
Scientific Paper | |
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Title | The Global Paleogeographical Reconstruction of the Triassic and the Paleoposiont of India |
Author(s) | Giancarlo Scalera |
Keywords | {{{keywords}}} |
Published | 1999 |
Journal | None |
Abstract
Following the production of a series of three paleogeographical reconstructions for the Paleocene, Cretaceous and Jurassic, a further reconstruction has been made here for the Triassic period, with the assistance of paleomagnetic data. The data provided by mutual fragment positions and paleomagnetic vectors, are best reconciled if the data is treated in an expanding Earth framework, and gives credence to the view that this represents the real evolution of the Earth. In particular a new solution of the case of Indian paleoposition is given which could constitute the key to the reinterpretation of the Eurasia paleogeography throughout geological time.