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- W2376469258 abstract "From systematic analysis and synthesis of geological surveying and geophysical exploring data, it is known that the central tectonic zone on the mainland of China is characterized by segmentation of active tectonics and various active crustal shortening structures. It is also demonstrated that its middle and southern segments are obstructing structural boundaries that consist of shallow and deep active compressional structures and obstruct the eastward or southeastward motion of the Qinghai-Tibetan Plateau at a lithospheric depth scale. There is an echoing relationship between the shallow and deep obstructing structures. Both of the shallow and deep compressional structures have partially transformed the eastward or southeastward motion of the blocks that are controlled by NW strike-slip faults into uplift of the eastern Qinghai-Tibetan Plateau. The synthetic study into the middle and southern segments as a whole will help us to understand the latest tectonic movement and also the dynamics of the earthquake migration in space and time on the mainland of China." @default.
- W2376469258 created "2016-06-24" @default.
- W2376469258 creator A5067057709 @default.
- W2376469258 date "2003-01-01" @default.
- W2376469258 modified "2023-09-25" @default.
- W2376469258 title "MODEL OF LATEST CRUSTAL TECTONIC MOTION OF THE CENTRAL TECTONIC ZONE ON THE MAINLAND OF CHINA" @default.
- W2376469258 hasPublicationYear "2003" @default.
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