| MECHANISM FOR CRUSTAL THICKENING IN TIBET: A PALEOMAGNETIC VIEW |
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| 引用本文： | Lin Jin-lu(Institute of Geology,Academia Sinica). MECHANISM FOR CRUSTAL THICKENING IN TIBET: A PALEOMAGNETIC VIEW[J]. 地震地质, 1987, 9(4): 49 |
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| 作者姓名： | Lin Jin-lu(Institute of Geology Academia Sinica) |
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| 作者单位： | Institute of Geology，Academia Sinica |
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| 摘 要： | The mid-Gretaceous paleomagnetic pole for the Lhasa Terrane (69.8°N 292.9°E, A95 = 5.1°) is in strong discordance with that for the stable Eurasia (69.5°N 167.4°E, A95 = 8.7°), which suggests that the Lhasa Terrane has moved 2400±800 km NNEward and rotated 31.4±9.2 counterclockwise with respect to the stable Eurasia. The relative motion started at the time when the Indian plate began to collide with the Eurasian plate (or maybe started a little earlier), and was accomplished through th
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MECHANISM FOR CRUSTAL THICKENING IN TIBET: A PALEOMAGNETIC VIEW |
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| Lin Jin-lu. MECHANISM FOR CRUSTAL THICKENING IN TIBET: A PALEOMAGNETIC VIEW[J]. Seismology and Geology, 1987, 9(4): 49 |
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| Authors: | Lin Jin-lu |
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| Abstract: | |
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| Keywords: | Tibetan Plateau Crustal shortening Crustal thickening Paleomagnetism Internal deformation within continents |
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