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

XIAO Long~1, WANG Fang-zheng~1, WANG Hua~2, F. Pirajno~3 1.Faculty of Earth Sciences, China University of Geosciences, Wuhan430074, China 2.Faculty of Earth Resources, China University of Geosciences, Wuhan430074, China 3.Geological Survey of Western Australia, 100 Plain Street, East Perth WA6004, Australia  
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.
【Fund】: 国家自然科学基金重点项目 (No .40 13 3 0 2 0 )
【CateGory Index】: P544.4
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