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- W2368376985 abstract "The Qinling mountains is a composite continental regime by distinct dynamics,and late orogenic tectonics in the north of the eastern Qinling orogenic belt is very important.The northern Qinling margin thrust structural zone in S→N direction is composed of two structural zones which are Yiyang-Lushan fault zone and Xiong'er rock sheet. Luanchuan-Funiu thrust structural zone in N→Sdirection has three zones, namely the front zone, the middle zone and the root zone. Machaoying strike-slip fault zone which is formed in the middle part of the north of the eastern Qinling is a positive flower structure. They were formed during late Yanshanian-early Himalayanian.It is the result of two-side-subduction of the Northern China plate and the Yangtze plate in the late orogenic period." @default.
- W2368376985 created "2016-06-24" @default.
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- W2368376985 date "2000-01-01" @default.
- W2368376985 modified "2023-09-25" @default.
- W2368376985 title "Late orogenic tectonics and forming mechanism in the north of Qinling-Dabie Mountains" @default.
- W2368376985 hasPublicationYear "2000" @default.
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