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- W2357190933 abstract "The erosion amounts of T 2 0, T 4 2 and T 0 3, three major Cenozoic regional unconformities in the Xihu Depression of the East China Sea, have been calculated by a number of approaches such as comprehensive stratigraphical correlation of balanced cross sections, acoustic moveout and hiatus of Ro methods. The erosion amounts of the three surfaces are generally distributed along the major tectonic belts of the Xihu Depression and local erosions are distributed in certain tectonic locations. The erosion model of T 0 2 has been identified as the slope-fold type and the erosion amount is mainly distributed along the central tectonic belt. The maximum erosion amount,more than 2000 m, lies along Wells Longjing 1, East Sea 1, Huagang 1, Yuquan 2 and Canxue 1.The erosion model of T 4 2 has been identified as the interim type and the erosion amount is mainly distributed on the eastern edge of the Xihu Depression. The Maximum erosion amount is more than 800 m. Local erosion is along such tectonic belts as East Sea 1, Longjing 1, Huagang 1, Yuquan 1, Yuquan 2, Canxue 1 and Chunxiao, and the average amount is 400～600 m. The erosion model of T 0 3 has been identified as the type of fault block-slope and the erosion amount is mainly distributed on the western slope, ranging from 200 to 800 m, and the local erosion is in the central tectonic belt, which is along the Longjing 2, Huagang 1, Yuquan 2, Tianwaitian 1 and the eastern tectonic belts, the average amount of which is less than 200～400 m." @default.
- W2357190933 created "2016-06-24" @default.
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- W2357190933 date "2005-01-01" @default.
- W2357190933 modified "2023-09-23" @default.
- W2357190933 title "Erosion Restoration of the Major Cenozoic Unconformities in the Xihu Depression of the East China Sea" @default.
- W2357190933 hasPublicationYear "2005" @default.
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