Trekking to the foot of Chomolungma (geological excursion in High Himalaya)
K.A. Novoselov, E.V. Belogub
UDК 551.1
Abstract
About autors
References
Abstract
The article deals with geological structure of the High Himalaya in traditional trekking route Lukla – base camp Chomolungma. The route crosses the sequence оf the highly metamorphosed rocks formed during the collision of the Indian and Tibetan plates.
Figures 2. References 37.
Key words: High Himalaya, Chomolungma.
About autors
K.A. Novoselov, Institute of Mineralogy UB RAS, Miass; const31@yandex.ru
E.V. Belogub, Institute of Mineralogy UB RAS, Miass
References
- Гансер А. Геология Гималаев. М.: Мир, 1967. 351 с.
- Rai S.M., Yoshida M., Upreti B.N., Ulak P.D. Geology of the Lesser Himalayan and Higher Himalayan Cristalline sequences of the Everest area along the Dudh Koshi valley, eastern Nepal Himalaya // Journal of Nepal Geological Society. 2007. Vol. 36. P. 11.
- Searly M., Simpson R., Law R., Parrish R., Waters D. The structural geometry, metamorphic and magmatic evolution of the Everest massif, High Himalaya of Nepal-South Tibet // Journal of the Geological Society. 2003. Vol. 160 (3). P. 345–366.
МINERALOGY № 3 2016