The structural geometry, metamorphic and magmatic evolution of the Everest massif, Nepal and South Tibet

The structural geometry, metamorphic and magmatic evolution of the Everest massif, Nepal and South Tibet

Two large scale, low-angle, north-dipping normal faults cut through the Everest massif, both faults being part of the South Tibetan Detachment (STD) system bounding the top of the southward extruding High Himalayan crustal wedge (Searle, 1999). The lower fault, the Lhotse detachment (LD) separates s...

Cur síos iomlán

Sonraí bibleagrafaíochta
Príomhchruthaitheoirí:	Searle, M, Simpson, R, Law, R, Parrish, R
Formáid:	Journal article
Teanga:	English
Foilsithe / Cruthaithe:	2001

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