Effect of Surface Morphology on the Dissipation During Shear and Slip Along a Rock–Rock Interface that Contains a Visco-elastic Core
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.springerlink.com/index/pdf/10.1007/s00024-011-0272-8
Reference28 articles.
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3. F. Arthaud and M. Mattauer. Exemples de stylolites d’origine tectonique dans le Languedoc, leur relation avec la tectonique cassante. Bulletin de la Société Géologique de France, 11:738–744, 1969.
4. J.S. Caine, J.P. Evans, and C.B. Forster. Fault zone architecture and permeability structure. Journal of Structural Geology, 24:1025–1028, 1996.
5. T. Candela, F. Renard, M. Bouchon, A. Brouste, D. Marsan, J. Schmittbuhl, and C Voisin. Characterization of fault roughness at various scales: Implications of three-dimensional high resolution topography measurements. Pure and Applied Geophysics, 166: doi: 10.1007/s00024-009-0521-2 , 2009.
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