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Numerical thermo-mechanical model predicts new observable magmatic and tectonic signatures for lithospheric delamination at active continental margins.

Authors
/persons/resource/stephan

Sobolev,  Stephan V.
Deutsches GeoForschungsZentrum;

/persons/resource/babeyko

Babeyko,  Andrey
Deutsches GeoForschungsZentrum;

/persons/resource/oncken

Oncken,  Onno
3.1 Lithosphere Dynamics, 3.0 Geodynamics and Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/bobby

Trumbull,  Robert
4.2 Inorganic and Isotope Geochemistry, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Citation

Sobolev, S. V., Babeyko, A., Oncken, O., Trumbull, R. (2004): Numerical thermo-mechanical model predicts new observable magmatic and tectonic signatures for lithospheric delamination at active continental margins., (EOS, Transactions, American Geophysical Union, Suppl.; Vol. 85, 47), AGU 2004 Fall Meeting (San Francisco 2004).


https://gfzpublic.gfz-potsdam.de/pubman/item/item_232252
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