Low-angle normal faults in the compressional Himalayan orogen; Evidence from the Annapurna-Dhaulagiri Himalaya, Nepal
The Annapurna Detachment (AD) is a lowangle (~20°-30° dip), north-dipping normal fault and ductile high-strain shear zone in calc-mylonites, and forms part of the South Tibetan Detachment (STD) that runs along 1800 km length of the Himalaya. The AD separates kyanite and sillimanite grade gneisses an...
| প্রধান লেখক: | |
|---|---|
| বিন্যাস: | Journal article |
| ভাষা: | English |
| প্রকাশিত: |
2010
|