Rheological weakening of subducted slabs due to the persistence of metastable 
olivine down to 600 km depth

Riedel, M. R.; Karato, S.; 2.1 Physics of Earthquakes and Volcanoes, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum

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Rheological weakening of subducted slabs due to the persistence of metastable olivine down to 600 km depth

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Riedel, M. R.
2.5 Geodynamic Modelling, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Karato, S.
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Riedel, M. R., Karato, S. (1997): Rheological weakening of subducted slabs due to the persistence of metastable olivine down to 600 km depth. - In: Upper Mantle Heterogeneities from Active and Passive Seismology, (NATO ASI series: Sub-series 1, Disarmament technologies ; 17), Dordrecht : Kluwer, 325-332.

Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_226146

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