A model of the crust and mantle structure down to 700 km depth beneath the Lhasa to Golmud transect across the Tibetan plateau as derived from seismological data
Author:
Funder
Deutsche Forschungsgemeinschaft
Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
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