Low-angle normal faults in the compressional Himalayan orogen; Evidence from the Annapurna-Dhaulagiri Himalaya, Nepal

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...

Cur síos iomlán

Sonraí bibleagrafaíochta
Príomhchruthaitheoir:	Searle, M
Formáid:	Journal article
Teanga:	English
Foilsithe / Cruthaithe:	2010

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