Ductile-brittle deformation in the hanging-wall of the South Tibetan Detachment System (Southern Tibet) (2008)

Please fill the following information to request the publication in hardcopy. We will get in touch with you shortly.

All form fields are required.

The South Tibetan Detachment System is characterised by a lower ductile shear zone, an upper  low-angle normal fault and high-angle normal faults. The low-angle normal fault puts in contact the base of the Tibetan Sedimentary Sequence with the high-grade sillimanite-bearing schists and mylonitic leucogranites of the Greater Himlayan Sequence and, in several places, the intervening North Col Formation. In the Rongbuck valley, Sa’er and Nyalam areas (southern Tibet) a sharp contact of the low-angle normal fault is associated to breccias and cataclasites.
Language: English
Imprint: Extended abstracts: 23rd Himalayan-Karakoram-Tibet Workshop, 2008, India. Himalayan Journal of Sciences Vol.5(7) (Special Issue) 2008 p.35: http://nepjol.info/index.php/HJS/article/view/1242/1222 2008
Series: Abstract,
Download: