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The geology of China (or the geological structure of the People's Republic of China) consists of three Precambrian cratons surrounded by a number of orogenic belts.The modern tectonic environment is dominated by the continued collision of India with the rest of Asia starting 40–50 million years ago.
During the 1952 reorganisation of Chinese higher education, Beijing Institute of Geology was founded as a result of the merger of several geology-related departments from Peking University, Tsinghua University, Tianjin University, and Tangshan Railway College. It was among China's first 16 key universities back in the 1950s.
Acta Sedimentologica Sinica (Chinese name: 沉积学报) is a peer-reviewed scientific journal covering the fields of sedimentology, sedimentary mineral deposits, and geochemistry. It is sponsored by the Professional Committee of Sedimentology of the Chinese Society of Mineral and Rock Geochemistry and the Professional Committee of Sedimentary ...
The journal was established in 1963 as Petroleum Geology Experiment Abstract (Chinese: 石油地质实验文摘) and renamed Experimental Petroleum Geology (Chinese: 石油地质实验) in 1965. [citation needed] In 1966, the journal ceased publication after three issues, but resumed publishing in 1978. [3]
Gondwana Research is a peer-reviewed scientific journal with an "all earth science" scope and an emphasis on the origin and evolution of continents. It is part of the Elsevier group, published by Journal Center, China University of Geosciences Beijing, 29 Xueyuan Road, Beijing 100083, China. [1]
The China Geological Survey (CGS) (Chinese: 中国地质调查局) is a government-owned, not-for-profit, Chinese organization researching China's mineral resources. It is a public institution managed by the State Council's ministries and commissions responsible for geological and mineral exploration under the State Council of the People's ...
Palaeoworld is a peer-reviewed academic journal with a focus on palaeontology and stratigraphy research in and around China. [2] It was founded in 1991 by the Nanjing Institute of Geology and Palaeontology at the Chinese Academy of Sciences (NIGPAS). [3]
The location of the Western Block of North China Craton is marked in red. Modified from Zhao, 2001. [1] The Western Block of the North China Craton is an ancient micro-continental block mainly composed of Neoarchean and Paleoproterozoic rock basement, with some parts overlain by Cambrian to Cenozoic volcanic and sedimentary rocks. [2]
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