Subducted crust and sediments - a source for intermediate depth earthquakes?.

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Behrmann, Jan Hinrich and Stipp, Michael (2007) Subducted crust and sediments - a source for intermediate depth earthquakes?. [Talk] In: EGU General Assembly. , 18.04, Vienna, Austria .

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Document Type: Conference or Workshop Item (Talk)
Research affiliation: OceanRep > SFB 574 > A1
OceanRep > SFB 574
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Refereed: No
Date Deposited: 03 Dec 2008 16:52
Last Modified: 06 Jul 2012 14:53
URI: https://oceanrep.geomar.de/id/eprint/1968

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