Add to ORKGMagnetotelluric models in northern Tibet are combined with laboratory studies. Constraints on melt fraction, temperature and crustal flow patterns are proposed. Discussion on proportion of crustal flow injected beneath the Kunlun fault
Gneiss domes involving the South Tibetan Detachment System provide evidence for crustal extension si...
Gneiss domes involving the South Tibetan Detachment System provide evidence for crustal extension si...
A total of 400 regional earthquakes were located in northern Tibetan Plateau from data recorded by I...
The overall objective of the final phase of the INDEPTH (International Deep Profiling of Tibet and H...
The weak lithosphere of the Tibetan plateau is surrounded by rigid crustal blocks1 and the transitio...
were re-analyzed and re-modelled in preparation for the MT Phase IV of the project focusing on the n...
The Kunlun fault defines one of the major northern tectonic boundaries of the Tibetan plateau. Previ...
One of the major geophysical discoveries concerning the Tibetan Plateau is the existence of unusuall...
There is considerable controversy over the nature of geophysically recognized low-velocity-high-cond...
The Tibetan Plateau is the largest orogenic system on Earth, and has been influential in our underst...
International audienceOver the past 70-50 Ma the Indo-Asian collision induced 1400 km of north-south...
Thesis (Ph. D.)--University of Washington, 2001This dissertation focus on the application of the mag...
P and S velocity and attenuation estimates in the lower crust are obtained from a set of wide angle ...
International audienceP and S velocity and attenuation estimates in the lower crust are obtained fro...
INDEPTH geophysical and geological observations imply that a partially molten mid-crustal layer exis...
Gneiss domes involving the South Tibetan Detachment System provide evidence for crustal extension si...
Gneiss domes involving the South Tibetan Detachment System provide evidence for crustal extension si...
A total of 400 regional earthquakes were located in northern Tibetan Plateau from data recorded by I...
The overall objective of the final phase of the INDEPTH (International Deep Profiling of Tibet and H...
The weak lithosphere of the Tibetan plateau is surrounded by rigid crustal blocks1 and the transitio...
were re-analyzed and re-modelled in preparation for the MT Phase IV of the project focusing on the n...
The Kunlun fault defines one of the major northern tectonic boundaries of the Tibetan plateau. Previ...
One of the major geophysical discoveries concerning the Tibetan Plateau is the existence of unusuall...
There is considerable controversy over the nature of geophysically recognized low-velocity-high-cond...
The Tibetan Plateau is the largest orogenic system on Earth, and has been influential in our underst...
International audienceOver the past 70-50 Ma the Indo-Asian collision induced 1400 km of north-south...
Thesis (Ph. D.)--University of Washington, 2001This dissertation focus on the application of the mag...
P and S velocity and attenuation estimates in the lower crust are obtained from a set of wide angle ...
International audienceP and S velocity and attenuation estimates in the lower crust are obtained fro...
INDEPTH geophysical and geological observations imply that a partially molten mid-crustal layer exis...
Gneiss domes involving the South Tibetan Detachment System provide evidence for crustal extension si...
Gneiss domes involving the South Tibetan Detachment System provide evidence for crustal extension si...
A total of 400 regional earthquakes were located in northern Tibetan Plateau from data recorded by I...