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- W2374097426 abstract "The vector map of crustal block’s motion in China Continent calculated from the long-term average slip rates of active faults and GPS survey data show that the eastward extrusion of the Qinghai-Xizang Plateau does exist, but its magnitude is not so large as that estimated by the continental escape hypothesis. The southern lateral extrusion boundary of the Plateau may consist of a set of discontinuous, scattered dextral strike-slip faults whose slip-rate is lower than 5 mm/a, rather than a continuous, single Karakoram-Jiali-Honghe fault zone. Chuandian(Sichuan-Yunnan) block is the most outstanding one among the lateral extrusion blocks in the Plateau, its south-south-eastward extrusion may be related to the difference between the lithospheric strength in Sichuan-Yunnan region." @default.
- W2374097426 created "2016-06-24" @default.
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- W2374097426 date "2003-01-01" @default.
- W2374097426 modified "2023-09-25" @default.
- W2374097426 title "ON THE LATERAL EXTRUSION OF SICHUAN-YUNNAN BLOCK (CHUANDIAN BLOCK)" @default.
- W2374097426 hasPublicationYear "2003" @default.
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