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Can intermediate depth earthquakes be caused by strain-hardening of SiO2 in subducted crust?.
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Stipp, Michael and Behrmann, Jan Hinrich (2007) Can intermediate depth earthquakes be caused by strain-hardening of SiO2 in subducted crust?. [Poster] In: Subduction Zone Geodynamics Conference. , 04.-07.06, Montpellier, France .
Full text not available from this repository.Document Type: | Conference or Workshop Item (Poster) |
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Research affiliation: | OceanRep > SFB 574 OceanRep > SFB 574 > A1 OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics |
Refereed: | No |
Date Deposited: | 03 Dec 2008 16:51 |
Last Modified: | 23 Sep 2019 23:46 |
URI: | https://oceanrep.geomar.de/id/eprint/5093 |
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