(Q59056199)

English

Implications of crustal property variations for models of Tibetan plateau evolution

scientific article published in Nature

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scholarly article

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Implications of crustal property variations for models of Tibetan plateau evolution (English)

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author name string

Thomas J. Owens

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George Zandt

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language of work or name

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publication date

May 1997

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387

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6628

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37-43

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https://scigraph.springernature.com/pub.10.1038/387037a0

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How flat is Tibet?

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A Review of Geophysical Constraints on the Deep Structure of the Tibetan Plateau, the Himalaya and the Karakoram, and their Tectonic Implications

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Deep seismic reflection evidence for continental underthrusting beneath southern Tibet

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Partially Molten Middle Crust Beneath Southern Tibet: Synthesis of Project INDEPTH Results

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Seismic anisotropy as an indicator of mantle flow beneath the Himalayas and Tibet

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Observations of regional phase propagation across the Tibetan Plateau

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Continental crust composition constrained by measurements of crustal Poisson's ratio

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Low crustal velocities and mantle lithospheric variations in southern Tibet from regional Pnl waveforms

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Lithospheric structure of Tibet and western North America: Mechanisms of uplift and a comparative study

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Mapping the descent of Indian and Eurasian plates beneath the Tibetan Plateau from gravity anomalies

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Thrust tectonics, deep structure and crustal subduction in the Alps and Himalayas

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Injection of Indian crust into Tibetan lower crust: A two-dimensional finite element model study

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Bright Spots, Structure, and Magmatism in Southern Tibet from INDEPTH Seismic Reflection Profiling

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INDEPTH Wide-Angle Reflection Observation of P-Wave-to-S-Wave Conversion from Crustal Bright Spots in Tibet

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Evidence from Earthquake Data for a Partially Molten Crustal Layer in Southern Tibet

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Electrically Conductive Crust in Southern Tibet from INDEPTH Magnetotelluric Surveying

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Evidence from gravity and topography data for folding of Tibet

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Upper mantle velocity structure beneath the Tibetan Plateau from Pn travel time tomography

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Timing of Tibetan uplift constrained by analysis of volcanic rocks

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Lattice preferred orientation of olivine aggregates deformed in simple shear

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Lateral extrusion of lower crust from under high topography in the isostatic limit

1 reference

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Some simple physical aspects of the support, structure, and evolution of mountain belts

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10.1038/387037A0

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