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- W2366568045 abstract "Huayingshan faults belt is an important boundary separating the ejective folds belt in east Sichuan basin and the flat zone of sichuan basin.Results from fault sliding and paleostress reconstruction indicate that there used to be three main periods of tectonic compression,that is the earlier S-N trending compression,the middle E-W trending compression and the later NE-SW trending compression which are related to the three major tectonic events respectively,the collision between North china block and yangtze block during Triassic,the uplifting of the Xuefeng mountain orogenic belts in the period of Yanshanian and the collision of India plate with Eurasiaplate in the period of Himalayan.The thrusting system to east sichuan basin was formed in the middle E-W trending compression event." @default.
- W2366568045 created "2016-06-24" @default.
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- W2366568045 date "2010-01-01" @default.
- W2366568045 modified "2023-09-23" @default.
- W2366568045 title "Fault sliding analysis and paleostress reconstruction of Huayingshan faults to East Sichuan basin" @default.
- W2366568045 hasPublicationYear "2010" @default.
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