Extensional and compressional faults in the Everest–Lhotse massif, Khumbu Himalaya, Nepal

Two large-scale north-dipping, low-angle normal faults cut the Everest massif at the top of the High Himalayan slab in Nepal. The upper fault the Qomolangma Detachment, follows the north slope of Everest from above the ‘Yellow Band’ at c. 8500 m on the Southwest Face down to the Rongbuk glacier. On...

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Bibliographic Details
Format: Journal article
Published: Geological Society Publishing House 1999
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