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The Tianshan and Junggar orogenic collage occupies the southwestern part of the Central Asian Orogenic Belt and was assembled by collision/accretion of several continental blocks and island arcs during late Paleozoic-early Mesozoic time, following the ...
Guochun Zhao, Yigui Han
exaly +4 more sources
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Central China Orogenic Belt and Amalgamation of East Asian Continents
Gondwana Research, 2021Abstract The Central China Orogenic Belt (CCOB) comprises, from the east to the west, the Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important amalgamation records of the North China, South China, Qaidam, Tarim and Qiangtang Blocks.
Jiaopeng Sun, Jie Zhao, Santosh M
exaly +2 more sources
A Review of the Paleozoic Tectonics in the Eastern Part of Central Asian Orogenic Belt
Gondwana Research, 2017Abstract The Central Asian Orogenic Belt (CAOB) is the largest accretionary orogen in the world, which is responsible for considerable Phanerozoic juvenile crustal growth. The NE China and its adjacent areas compose the eastern segment of the CAOB, which is a key area for providing important evidence of the CAOB evolution and understanding the NE ...
Franz Neubauer +2 more
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International audienceBased mainly on field geological observation and geochronologic data, six tectonic units have been recognized in western Inner Mongolia (China), including, from south to north: North China Craton (NCC), Southern Orogenic Belt (SOB),
Yan Chen, Pan Zhao
exaly +2 more sources
Lithos, 2018
Abstract The Beishan Orogenic Belt is located in the central southernmost part of the Central Asian Orogenic Belt (CAOB), which plays a key role in understanding the formation and evolution of the CAOB. Granitoids are the documents of crustal and tectonic evolution in orogenic belts.
Zhaochu Hu, Zhenyu He, Zeming Zhang
exaly +2 more sources
Abstract The Beishan Orogenic Belt is located in the central southernmost part of the Central Asian Orogenic Belt (CAOB), which plays a key role in understanding the formation and evolution of the CAOB. Granitoids are the documents of crustal and tectonic evolution in orogenic belts.
Zhaochu Hu, Zhenyu He, Zeming Zhang
exaly +2 more sources
The Western Central Asian Orogenic Belt: A Window to Accretionary Orogenesis and Continental Growth
Gondwana Research, 2014Santosh M, Wenjiao Xiao
exaly

