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Comparisons of the kinematics and deep structures of the Zagros and Himalaya and of the Iranian and Tibetan plateaus and geodynamic implications
D Hatzfeld, P Molnar - Reviews of Geophysics, 2010 - Wiley Online Library
We compare the geologic histories, the deep structures, and the present‐day kinematics of
deformation of the Himalaya and the adjacent Tibetan Plateau with those of the Zagros and …
deformation of the Himalaya and the adjacent Tibetan Plateau with those of the Zagros and …
A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion
Using data from more than 2000 seismic stations from multiple networks arrayed throughout
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …
Uplift of the Longmen Shan and Tibetan plateau, and the 2008 Wenchuan (M = 7.9) earthquake
Abstract The Longmen Shan mountain range, site of the devastating 12 May 2008
Wenchuan (M= 7.9) earthquake, defines the eastern margin of the Himalayan orogen and …
Wenchuan (M= 7.9) earthquake, defines the eastern margin of the Himalayan orogen and …
Subduction of the Indian lithosphere beneath the Tibetan Plateau and Burma
Subduction of the Indian lithosphere under Eurasia plays an important role in the tectonic
evolution of the Tibetan plateau and surrounding regions. To improve our knowledge of …
evolution of the Tibetan plateau and surrounding regions. To improve our knowledge of …
[كتاب][B] Global tectonics
P Kearey, KA Klepeis, FJ Vine - 2009 - books.google.com
The third edition of this widely acclaimed textbook provides a comprehensive introduction to
all aspects of global tectonics, and includes major revisions to reflect the most significant …
all aspects of global tectonics, and includes major revisions to reflect the most significant …
A synoptic view of the distribution and connectivity of the mid‐crustal low velocity zone beneath Tibet
Based on 1–2 years of continuous observations of seismic ambient noise data obtained at
more than 600 stations in and around Tibet, Rayleigh wave phase velocity maps are …
more than 600 stations in and around Tibet, Rayleigh wave phase velocity maps are …
Crustal flow pattern beneath the Tibetan Plateau constrained by regional Lg-wave Q tomography
As a prominent geophysical anomaly, unusually high seismic wave attenuation is observed
in the crust and upper mantle of the Tibetan Plateau, particularly along its northern area …
in the crust and upper mantle of the Tibetan Plateau, particularly along its northern area …
Convective removal of the Tibetan Plateau mantle lithosphere by~ 26 Ma
During the late Oligocene–early Miocene there were several major geological events in and
around the Tibetan Plateau (TP). First, crustal shortening deformation ceased completely …
around the Tibetan Plateau (TP). First, crustal shortening deformation ceased completely …
Thinning and flow of Tibetan crust constrained by seismic anisotropy
Intermediate-period Rayleigh and Love waves propagating across Tibet indicate marked
radial anisotropy within the middle-to-lower crust, consistent with a thinning of the middle …
radial anisotropy within the middle-to-lower crust, consistent with a thinning of the middle …
Lithospheric thickness of the Chinese continent
We invert for the upper-mantle temperatures of the Chinese continent in the depth range of
70–240km from a recent S-velocity model. The depth where temperatures intersect a mantle …
70–240km from a recent S-velocity model. The depth where temperatures intersect a mantle …