THE FORMATION OF BOHAI SEA AND ITS DEEP DYNAMICS

NIU Shuyin; SUN Aiqun; WANG Mengke; ZUO Liming; ZHANG Xunhua; ZHANG Fuxiang; HOU Jianglong; XU Meng; ZHANG Jianzhen; CHEN Chao

doi:10.3724/SP.J.1140.2014.06063

2014 Vol. 34, No. 6

Article Contents

Abstract

References

Article navigation > Marine Geology & Quaternary Geology > 2014 > 34(6): 63-71

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NIU Shuyin, SUN Aiqun, WANG Mengke, ZUO Liming, ZHANG Xunhua, ZHANG Fuxiang, HOU Jianglong, XU Meng, ZHANG Jianzhen, CHEN Chao. THE FORMATION OF BOHAI SEA AND ITS DEEP DYNAMICS[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 63-71. doi: 10.3724/SP.J.1140.2014.06063

Citation:

NIU Shuyin, SUN Aiqun, WANG Mengke, ZUO Liming, ZHANG Xunhua, ZHANG Fuxiang, HOU Jianglong, XU Meng, ZHANG Jianzhen, CHEN Chao. THE FORMATION OF BOHAI SEA AND ITS DEEP DYNAMICS[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 63-71. doi: 10.3724/SP.J.1140.2014.06063

THE FORMATION OF BOHAI SEA AND ITS DEEP DYNAMICS

1. Shijiazhuang University of Economics, College of Resources, Shijiazhuang, Hebei 050031, China;
2. Hebei Bureau of Geology and Mineral Resources, Institute of Hydrologic and Engineering Geology, Shijiazhuang 050021, China;
3. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071

Received Date: 21 March 2014

Revised Date: 29 March 2014

Abstract

Abstract

Starting from the Yanshan movement, the tectonic system in the east part of North China has suffered drastic changes.The tectonic regime of the region changed from the merge of terranes and continent accretion of the Indo-Sinian period into the evolution of mantle plume marked by the extensional rifting of the Bohai basin in the later stage. The topography of the legion is also changed from a uplifting plateau to a basin-range system in the east of North China, with the Bohai mantle plume remained in the center characterized by large-scale rifting and series of mantle branches in the periphery. The formation of the Bohai Sea is the result of mantle plume evolution in the shallow part, which caused strong tectonic movement, magmatism and regional ultrametamorphismin in the whole region during the Yanshan-Himalayan period.
- mantle crust movement /
- mantle plume /
- mantle branch structure /
- extensional tectonics /
- basin range coupling /
- the Bohai Sea

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References

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