Giant rockslides from the inside-Reference-Cited by-同舟云学术

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Giant rockslides from the inside

Published:2014-03 Issue: Volume:389 Page:62-73
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Weidinger Johannes T.,Korup Oliver,Munack Henry,Altenberger Uwe,Dunning Stuart A.,Tippelt Gerold,Lottermoser Werner

Funder

European Commission

German Research Foundation

DFG

Potsdam Research Cluster for Georisk Analysis, Environmental Change and Sustainability (PROGRESS)

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference66 articles.

1. Large rockslides: their causes and movement on internal sliding planes;Abele;Mt. Res. Dev.,1994

2. Garnet-bearing pseudotachylytes of Calabria – a petrological link to lower crustal hypocenters;Altenberger;Geol. Soc. (Lond.) Spec. Publ.,2011

3. A seismogenic zone in the lower crust indicated by pseudotachylytes and ultramylonites in granulite-facies rocks of Calabria (southern Italy);Altenberger;Contrib. Mineral. Petrol.,2013

4. Grain size distribution and thickness of breccia and gouge zones from thin (<1 m) strike-slip fault cores in limestone;Billi;J. Struct. Geol.,2005

5. Fractal distribution of particle size in carbonate cataclastic rocks from the core of a regional strike-slip fault zone;Billi;Tectonophysics,2004

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