Triaxial deformation experiments indicate strong sediments at the deformation front, and weak sediments at the rear of the Nankai accretionary prism.

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Stipp, Michael, Rolfs, Malte, Kitamura, Yujin and Behrmann, Jan H. and GEOMAR, Helmholtz-Zentrum für Ozeanforschung Kiel, Instiut für Geowissenschaften, Universität Kiel (2012) Triaxial deformation experiments indicate strong sediments at the deformation front, and weak sediments at the rear of the Nankai accretionary prism. [Poster] In: 14. Symposium on Tectonics, Structural Geology and Geology of Crystalline Rocks (TSK 14). , 28.03.-30.03.2012, Kiel . 14. Symposium: Tectonics, Structural Geology and Geology of Crystalline Rocks = Tektonik, Strukturgeologie und Kristallingeologie : Kiel 26.3.-1.4.2012 ; program, abstracts. ; p. 95 .

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Document Type: Conference or Workshop Item (Poster)
Additional Information: Buch vorhanden in der GEOMAR-Bibliothek / Book in stock in the GEOMAR Library: GEOL-TEK 99-1
Keywords: Geodynamics; Geology
Research affiliation: Kiel University
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Publisher: The Future Ocean
Related URLs:
Date Deposited: 18 Jul 2012 12:30
Last Modified: 23 Sep 2019 22:13
URI: https://oceanrep.geomar.de/id/eprint/14858

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