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Tectonics of the Tian Shan information


A regional map highlighting the relative locations of major orogenic belts in central Asia.
West Tian Shan mountains

The Tian Shan is a mountain range in central Asia that extends through western China, Kazakhstan, and Kyrgyzstan.[1] The Tian Shan is 2,800 kilometres (1,700 mi) long, and up to 7,400 metres (24,300 ft) high. Throughout the Tian Shan there are several intermontane basins separated by high ranges.[1] Plate tectonic theory makes the assumption that deformation is concentrated along plate boundaries. However, active deformation is observed in the Tian Shan, far from plate boundaries. This apparent contradiction of plate tectonic theory makes the Tian Shan a key place to study the dynamics of intracontinental deformation.[2]

  1. ^ a b Cite error: The named reference Jolivet was invoked but never defined (see the help page).
  2. ^ Cite error: The named reference Wang11 was invoked but never defined (see the help page).

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Tectonics of the Tian Shan

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and Cenozoic Tectonic History of the Central Chinese Tian Shan: Reactivated Tectonic Structures and Active Deformation" (PDF). Tectonics. 29 (6): 1–30...

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Tian Shan

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The Tian Shan (Chinese: 天山), also known as the Tengri Tagh or Tengir-Too, meaning the "Mountains of God/Heaven", is a large system of mountain ranges...

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Junggar Basin

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by the Tarbagatai Mountains of Kazakhstan in the northwest, the Altai Mountains of Mongolia in the northeast, and the Heavenly Mountains (Tian Shan) in...

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Tectonic uplift

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Tectonic uplift is the geologic uplift of Earth's surface that is attributed to plate tectonics. While isostatic response is important, an increase in...

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Kolsay Lakes National Park

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the north slope of the Tian Shan Mountains, southeast Kazakhstan (10 km from the border with Kyrgyzstan). Often referred to as "Pearls of Tien Shan"...

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Bayanbulak Grassland National Nature Reserve

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"abundant spring") is the second largest grassland in China, located in the Bayanbulak Basin of the Tian Shan mountains in northwest China. The terrain is mostly...

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Mount Tai

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(Chinese: 泰山; pinyin: Tài Shān) is a mountain of historical and cultural significance located north of the city of Tai'an. It is the highest point in Shandong...

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Pamir Mountains

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namely the Tian Shan, Karakoram, Kunlun, Hindu Kush and the Himalaya mountain ranges. They are among the world's highest mountains. Much of the Pamir Mountains...

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Foreland basin

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Pro-foreland to the south of the Tian Shan Formed initially during the Late Paleozoic, during the Carboniferous and Devonian Rejuvenated during the Cenozoic...

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1887 Verny earthquake

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Yoshiki Ninomiya; Jianming Guo (2010). "Slip partitioning in the northeast Pamir–Tian Shan convergence zone" (PDF). Tectonophysics. 483 (3–4): 344–364...

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Mantle convection

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PMID 14657505. S2CID 35802740. Small-scale convection in the upper mantle beneath the Chinese Tian Shan Mountains, http://www.vlab.msi.umn...

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1911 Kebin earthquake

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Djanuzakov, K.D.; Delvaux, D. (2002). "Active tectonics and seismic hazard of the Issyk-Kul Basin in the Kyrgyz Tian-Shan". In Klerkx J.; Imanackunov B. (eds.)...

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Alpide belt

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Mount Ida; Caucasus Mountains (on the limits between Asia and Europe), Kopet Mountains, Pamir, Alay Mountains, Tian Shan, Altai Mountains, Sayan Mountains;...

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Xinjiang

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India. The rugged Karakoram, Kunlun and Tian Shan mountain ranges occupy much of Xinjiang's borders, as well as its western and southern regions. The Aksai...

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Dzungaria

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that corresponds to the northern half of Xinjiang. Bound by the Altai Mountains to the north and the Tian Shan mountain range to the south, Dzungaria covers...

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2020 Kashgar earthquake

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"Late Cenozoic tectonics of the Kepingtage thrust zone: Interactions of the Tien Shan and Tarim Basin, northwest China". Tectonics. 18 (4): 639–654...

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Variscan orogeny

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include the Urals, the Pamir, the Tian Shan and other Asian foldbelts. The Variscan orogeny involved a complicated heterogeneous assembly of different microplates...

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North Asia

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found on the east Siberian mountains, on the mountains of the Kamchatka Peninsula, on the Altai, on Tian Shan, and on other small areas of mountains...

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1946 Chatkal earthquake

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earthquake, the largest in the republic since 1911. The earthquake's hypocenter is probably located beneath the Tian Shan Mountains, near the border with Uzbekistan...

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1906 Manasi earthquake

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Zhuohui; Fang, Lihua (2019). "The 2016 Mw 6.0 Hutubi earthquake: A blind thrust event along the northern Tian Shan front". Journal of Asian Earth Sciences. 173:...

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1902 Turkestan earthquake

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in the Tien Shan mountains. The thrust earthquake measured 7.7 on the moment magnitude scale (Mw ) and had a depth of 18 km (11 mi). The Tien Shan mountains...

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List of mountain ranges

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(1993). "High cooling and denudation rates at Kongur Shan, Eastern Pamir (Xinjiang, China)". Tectonics. 12 (3): 1335–1346. doi:10.1029/93TC00767.{{cite journal}}:...

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Geology of China

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Xianglin, Qian; Geng, Yang (1998). "Late Cenozoic tectonic evolution of the southern Chinese Tian Shan". Tectonics. 17 (1): 1–27. Bibcode:1998Tecto..17....1Y...

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Manas Lake

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in the past. Notionally, Lake Manas is considered the end point of the Manas River, flowing from the Tian Shan mountains. In practice, however, the river...

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Geology of Kyrgyzstan

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The geology of Kyrgyzstan began to form during the Proterozoic. The country has experienced long-running uplift events, forming the Tian Shan mountains...

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Uralian orogeny

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in the Early Jurassic. The southern continuation of the Ural mountains, the southern Tian-Shan mountains, formed in the late Palaeozoic with the closure...

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North China Craton

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atmospheric and hydrosphere interaction and the evolution from primitive tectonics to modern plate tectonics. Ore formation is related to supercontinent...

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Intraplate deformation

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the Tibetan Plateau (Figure 1). Intraplate deformation brings another aspect to plate tectonic theory. The theory of plate tectonics states that the Earth's...

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1889 Chilik earthquake

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Yoshiki Ninomiya; Jianming Guo (2010). "Slip partitioning in the northeast Pamir–Tian Shan convergence zone" (PDF). Tectonophysics. 483 (3–4): 344–364...

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