地幔柱构造对松辽盆地及渤海湾盆地形成的制约

肖龙; 王方正; 王华; PirajnoF.

Volume 29 Issue 3

May 2004

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XIAO Long, WANG Fang-zheng, WANG Hua, Pirajno F., 2004. Mantle Plume Tectonics Constraints on the Formation of Songliao and Bohaiwan Basins. Earth Science, 29(3): 283-292.

Citation:

XIAO Long, WANG Fang-zheng, WANG Hua, Pirajno F., 2004. Mantle Plume Tectonics Constraints on the Formation of Songliao and Bohaiwan Basins. Earth Science, 29(3): 283-292.

XIAO Long, WANG Fang-zheng, WANG Hua, Pirajno F., 2004. Mantle Plume Tectonics Constraints on the Formation of Songliao and Bohaiwan Basins. Earth Science, 29(3): 283-292.

Citation:

XIAO Long, WANG Fang-zheng, WANG Hua, Pirajno F., 2004. Mantle Plume Tectonics Constraints on the Formation of Songliao and Bohaiwan Basins. Earth Science, 29(3): 283-292.

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Mantle Plume Tectonics Constraints on the Formation of Songliao and Bohaiwan Basins

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
Geological Survey of Western Australia, 100 Plain Street, East Perth WA 6004, Australia

Received Date: 2003-10-23
Publish Date: 2004-05-25

Abstract

Abstract

The dynamic mechanisms of the formation of the Songliao and the Bohaiwan basins, eastern China, are controversial. Based on the analyses of earthquake data, sedimentary record, volcanic probe and tectonic evolution, it is argued that the activity of mantle plume firstly undertook at the region around the Songhuajiang and the Liaohe rivers during Late Jurassic and Early Cretaceous time. The plume head was of 500 km in diameter at this stage. The Songliao basin formed due to the asthenospheric upwelling, crustal uplift and subsequent extension, and volcanic activity. However, the mantle plume, with 600-800 km head in diameter, would be beneath the Bohaiwan area in the Paleocene due to northwestward movement of the North China plate. The similar geological processes to the last stage undertook, and resulted in the formation of the Bohaiwan basin. Meanwhile, the plume is interpreted as the major factor of frequent earthquake at the Beijing-Tianjin and Bohaiwan area.
- mantle plume,
- mantle plume tectonics,
- Songliao basin,
- Bohaiwan basin,
- volcanism,
- earthquake.

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References(75)

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Mantle Plume Tectonics Constraints on the Formation of Songliao and Bohaiwan Basins

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