Seismic imaging of subducting continental lower crust beneath the Pamir
Exhumation of ultra-high pressure metamorphic rocks testifies that the continental crust can subduct to significant depth into the mantle despite its buoyancy. However, direct observation of ongoing subduction of continental crust is rare. The Pamir is re
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|Source:||Earth and Planetary Science Letters|
|01_Schneider_Seismic_imaging_of_subducting_2013.pdf||855.51 kB||Adobe PDF||Request a copy|
|02_Schneider_Seismic_imaging_of_subducting_2013.pdf||856.28 kB||Adobe PDF||Request a copy|
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