Deep crustal deformation of the Longmen Shan, eastern margin of the Tibetan Plateau, from seismic reflection and Finite Element modeling

Rivaling the Himalaya in relief, the Longmen Shan is probably one of the most enigmatic mountain ranges in the world: high mountains reach more than 4000 m relief but without adjacent foreland subsidence and with only slow active convergence. What are geological and geodynamic processes that built t...

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Veröffentlicht in:	Journal of geophysical research. Solid earth 2016-02, Vol.121 (2), p.767-787
Hauptverfasser:	Feng, Shao‐ying, Zhang, Pei‐zhen, Liu, Bao‐jin, Wang, Ming, Zhu, Shou‐biao, Ran, Yong‐kan, Wang, Wei‐tao, Zhang, Zhu‐qi, Zheng, Wen‐jun, Zheng, De‐wen, Zhang, Hui‐ping, Tian, Xiao‐feng
Format:	Artikel
Sprache:	eng
Schlagworte:	Brittleness Contraction Convergence Crustal deformation Crusts deep seismic sounding Deformation Deformation mechanisms Depth profiling Dipping Displacement Ductile brittle transition ductile shear zone Earthquake construction Earthquakes Fault lines Faults Finite element method Flexing Formability Geological faults Geology Geophysics listric reverse fault Longmen Shan Magma Mantle Mathematical analysis Mathematical models Modelling Mountains Plateaus Profiling Reflection Reflectors Rupture Seismic activity Seismic reflection profiling Seismic surveys Shear Shearing Slip Sounding Subsidence Tibetan Plateau Viscoelasticity Wenchuan earthquake
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