Fault system in the Himalayan region across India and Asia
The Karakoram fault is an oblique-slip fault system in the Himalayan region across India and Asia. The slip along the fault accommodates radial expansion of the Himalayan arc,[2] northward indentation of the Pamir Mountains,[3] and eastward lateral extrusion of the Tibetan plateau.[4][5] Current plate motions suggest that the convergence between the Indian Plate and the Eurasian Plate is around 44±5 mm per year in the western Himalaya-Pamir region and approximately 50±2 mm per year in the eastern Himalayan region.[6]
^Cite error: The named reference Murphy, et al., 2000 was invoked but never defined (see the help page).
^Murphy, M. A.; P. Copeland (2005). "Transtentional deformation in the central Himalay and its role in accommodating growth of the Himalayan orogeny". Tectonics. 24 (4): n/a. Bibcode:2005Tecto..24.4012M. doi:10.1029/2004TC001659. S2CID 106406740.
^Sobel, E. R.; L. M. Schoenbohm; J. Chen; R. Thiede; D. F. Stockli; M. Sudo; M. R. Strecker (2011). "Late Miocene-Pliocene deceleration of dextral slip between Pamir and Tarim: Implications for Pamir orogensis". Earth and Planetary Science Letters. 304 (3–4): 369–378. Bibcode:2011E&PSL.304..369S. doi:10.1016/j.epsl.2011.02.012.
^Cite error: The named reference Searle, 1996 was invoked but never defined (see the help page).
^Murphy, Mike A.; A. Yin; P. Kapp; T. M. Harrison; C. E. Manning (2002). "Isotopic characteristics of the Gurla Mandhata metamorphic core complex: Implications for the architecture of the Himalayan orogen". Geology. 35 (114): 428–447. doi:10.1130/G23774A.1.
The Karakoramfault is an oblique-slip faultsystem in the Himalayan region across India and Asia. The slip along the fault accommodates radial expansion...
Suture Zone Transhimalaya, includes the following two Lhasa terrane Karakoramfaultsystem Bangong-Nujiang Suture Zone Qiangtang terrane Look up Transhimalaya...
is causing rapid uplifting of lower crustal rocks Karakoramfaultsystem - major active faultsystem within the Himalayas Mount Everest Paleotethys Sutlej...
(also discussed in Geography of Tibet) Paleotethys Karakoramfaultsystem - major active faultsystem within the Himalaya Main Himalayan Thrust - the root...
subdivisions of Himalayas (from north to south) Indus-Yarlung suture zone Karakoramfaultsystem Nyenchen Tanglha Mountains Main Himalayan Thrust Lower/Lesser Himalaya...
that runs for over 850 km. Tectonically, it is actually a system of related geologic faults that separates the Eurasian Plate from the Indo-Australian...
Peak (Rupal Valley) Shaigiri Geology of the Himalaya Karakoramfaultsystem - major active faultsystem within the Himalayas List of highest mountains on...
Himalaya Indus Suture Zone Transhimalaya, includes Lhasa terrane and Karakoramfaultsystem High pressure metamorphic terranes along the Bangong-Nujiang Suture...
This list covers all faults and fault-systems that are either geologically important[clarification needed] or connected to prominent seismic activity.[clarification...
Matterhorn of the East Nyenchen Tanglha. Transhimalaya Lhasa terrane Karakoramfaultsystem Geology of the Himalaya The Trans-Himalaya, named by Sven Hedin...
of 17 ± 2 mm/yr along the Main Himalayan Thrust while the nearby Karakoramfaultsystem accommodates right-lateral strike-slip movement at 5 ± 2 mm/yr....
Indus Suture Zone Transhimalaya, includes following: Lhasa terrane Karakoramfaultsystem High pressure metamorphic terranes along the Bangong-Nujiang Suture...
is now recognized as a geological fault called the Longmu Co fault, part of the larger Longmu–Guozha Co faultsystem. The Chang Chenmo River has its origin...
intersection of two major strands of the Karakoramfaultsystem, called the Tangtse fault and the Pangong fault. The two faults sandwich the Pangong Range, at the...
of 17 ± 2 mm/yr along the Main Himalayan Thrust while the nearby Karakoramfaultsystem accommodates right-lateral strike-slip movement at 5 ± 2 mm/yr....
the Karakoram range, partially in the Gilgit-Baltistan region of Pakistan-administered Kashmir and partially in the China-administered Trans-Karakoram Tract...
large-scale movements of the Earth's crust (tectonic plates). Folding, faulting, volcanic activity, igneous intrusion and metamorphism can all be parts...
higher. The highest cliff in the solar system may be Verona Rupes, an approximately 20 km (12 mi) high fault scarp on Miranda, a moon of Uranus. The...
coastal areas of the Indian Ocean in the south to the mountains of the Karakoram, Hindukush, Himalayas ranges in the north. Pakistan geologically overlaps...
Harish Kapadia (1999). Across Peaks & Passes in Ladakh, Zanskar & East Karakoram. Indus Publishing. p. 230. ISBN 978-81-7387-100-9. Shyok: river of death...
Pakistan, and China. The Himalayan range is bordered on the northwest by the Karakoram and Hindu Kush ranges, on the north by the Tibetan Plateau, and on the...
Caucasus, the Alborz, the Zagros, the Hajar, the Hindu Kush, the Pamir, the Karakoram, and the Himalayas. Sometimes other names occur to describe the formation...
Chile and Argentina. Such mountain systems have a complex structure, which is usually the result of folding and faulting accompanied by volcanic activity...
Himalayas (from Brahmaputra River in the east to Indus River in the west), Karakoram (from Indus River in the east to Yarkand River in the west) and the Hindu...
of the India–Asia collision. These faults, including the Altyn Tagh, Haiyuan, Kunlun, Karakoram and Xianshuihe faults, accommodate crustal deformation within...
China, Bhutan, and Nepal. Its western border with Pakistan lies in the Karakoram and Western Himalayan ranges, Punjab Plains, the Thar Desert and the Rann...
89.34°E / 42.78; 89.34 The Turpan Depression or Turfan Depression, is a fault-bounded trough located around and south of the city-oasis of Turpan, in...
processes in the construction and evolution of Oman-, Zagros-, Himalayan-, Karakoram-, and Tibetan type orogenic belts". In Robert D. Hatcher Jr.; MP Carlson;...