Tectonic evolution of the central Annapurna Range, Nepalese Himalayas
The metamorphic core of the Himalayan orogen, or Greater Himalayan sequence, is a northward tapering prism bound at the bottom by a N dipping family of thrust faults (the Main Central thrust system) and at the top by a N dipping family of normal faults (the South Tibetan detachment system). Research...
| Main Authors: | , , |
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| 格式: | Journal article |
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1996
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