Diagenetic facies and pore evolution of tight sandstone reservoirs of the Jiamuhe formation in the Shawan sag, Junggar basin. [PDF]
Zongquan Y +9 more
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Oxidized sediment recycling as a driver for postsubduction porphyry copper formation. [PDF]
Yang Z +7 more
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Devonian-Mississippian magmatism related to extensional collapse in Svalbard: implications for radiating dyke swarms. [PDF]
Koehl JP, Tappe S, Foulger GR, Anell IM.
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The crustal juvenile and reworking in eastern Tibet due to tectonism and magmatism. [PDF]
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Organic matter accumulation under the Middle-Upper Ordovician tectonic transition on the western margin of the North China platform. [PDF]
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Characterization and regional variations in the mineralogical maturity of aeolian sands in northern China. [PDF]
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Identification of Geochemical Anomalies Based on RPCA and Multifractal Theory: A Case Study of the Sidaowanzi Area, Chifeng, Inner Mongolia. [PDF]
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Late Paleozoic paleomagnetic constraints on the eastern segment of the Central Asian Orogenic Belt
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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.
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Abstract The formation of the Central Asian Orogenic Belt is thought to be related to the evolution of the Paleo-Asian Ocean surrounded by the Siberian, European, and Tarim-North China cratons. The West Junggar Orogenic Belt (WJOB) in the southern Central Asian Orogenic Belt is part of the Kazakhstan-Junggar terrane between the Altay Orogenic Belt to
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