Normal faulting and viscous buckling in the Tibetan Plateau induced by a weak lower crust
نویسندگان
چکیده
منابع مشابه
Seismic Imaging of Microblocks and Weak Zones in the Crust Beneath the Southeastern Margin of the Tibetan Plateau
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15 صفحه اولStructure of the crust beneath the southeastern Tibetan Plateau from teleseismic receiver functions
Southeastern Tibet marks the site of presumed clockwise rotation of the crust due to the India–Eurasian collision and abutment against the stable Sichuan basin and South China block. Knowing the structure of the crust is a key to better understanding of crustal deformation and seismicity in this region. Here, we analyze recordings of teleseismic earthquakes from 25 temporary broadband seismic s...
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ژورنال
عنوان ژورنال: Nature Communications
سال: 2018
ISSN: 2041-1723
DOI: 10.1038/s41467-018-07312-9