Experimental modeling of strike-slip faults and the self-similar behavior

Author(s)
M.P.J. Schöpfer, H.P. Steyrer
Abstract

Analogue modeling of strike-slip faults in sandbox experiments gave new insights into the nature of the relationship between size of structures and the thickness of the granular material. Experiments have been conducted with different materials and varying thicknesses. The results emphasize the self-similar behavior of structures modeled in sandbox experiments. Shearing of the sand cake led to a change of the sand properties, such as the frictional angle and the packing density within the shear-zone. Dilatancy is an undesirable effect and a scaling problem. Supressing dilatancy by the use of coarse-grained granular material consisting of well-rounded grains with smooth surfaces led to quasiductile behavior of the shear-zone. Layered models with quasiductile granular material and typical model sand led to results similar to those observed in prestressed sand cakes.

Organisation(s)
Department of Geology
External organisation(s)
Paris-Lodron Universität Salzburg
Journal
Memoirs of the Geological Society of America
Volume
193
Pages
21-27
No. of pages
7
ISSN
0072-1069
DOI
https://doi.org/10.1130/0-8137-1193-2.21
Publication date
01-2001
Peer reviewed
Yes
Portal url
https://ucrisportal.univie.ac.at/en/publications/c559eb09-9fb1-4cd0-a2f5-20cef3d4994a