关于发展洋板块地质学的思考

李廷栋; 肖庆辉; 潘桂棠; 陆松年; 丁孝忠; 刘勇

doi:10.3799/dqkx.2019.970

Volume 44 Issue 5

May 2019

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Article Navigation > Earth Science > 2019 > 44(5): 1441-1451

Li Tingdong, Xiao Qinghui, Pan Guitang, Lu Songnian, Ding Xiaozhong, Liu Yong, 2019. A Consideration about the Development of Ocean Plate Geology. Earth Science, 44(5): 1441-1451. doi: 10.3799/dqkx.2019.970

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Li Tingdong, Xiao Qinghui, Pan Guitang, Lu Songnian, Ding Xiaozhong, Liu Yong, 2019. A Consideration about the Development of Ocean Plate Geology. Earth Science, 44(5): 1441-1451. doi: 10.3799/dqkx.2019.970

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A Consideration about the Development of Ocean Plate Geology

doi: 10.3799/dqkx.2019.970

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Information Center of Ministry of Natural Resources of People's Republic of China, Beijing 100830, China
3.
Chengdu Geological Survey Center, China Geological Survey, Chengdu 610081, China
4.
Tianjin Geological Survey Center, China Geological Survey, Tianjin 300170, China
5.
Hebei University of Geosciences, Shijiazhuang 050031, China

Received Date: 2019-01-06
Publish Date: 2019-05-15

Abstract

Abstract

In order to reveal the material composition and the structure of the orogenic belt, we propose the ocean plate geology, which is used to explain the process of continental formation and evolution and the source of dynamics. Based on the theory of plate tectonics and geological research methods, the subduction-accretionary complex, the ophiolite belt, and other oceanic lithospheric plate geological formations and structure construction in the orogenic belt are systematically studied in order to find the igneous rock association of the front arc in the subduction zone. In the initial subduction process of the ocean plate, the magmatism from the forearc basalts (FAB) to the boninite, high-Mg andesite (HMA), to the arc tholeiite and calc-alkaline lava and its different stage evolution, are studied in order to identify the characteristics of the original arc and front arc igneous rock association, which reveals the ocean-continent transition in the evolution process from ocean basin to the continent, laying a scientific foundation for the establishment and development of ocean plate geology.
- ocean plate geology,
- subduction-accretionary complex,
- intra-oceanic arc,
- ocean-continent transition,
- tectonics

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References(56)

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A Consideration about the Development of Ocean Plate Geology

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