Grain size distributions of fault rocks: A comparison between experimentally and naturally deformed granitoids
We have investigated the grain size distribution (GSD) of granitoid fault rock by comparing experimentally produced gouge with fault rock from the Nojima Fault Zone. Triaxial experiments were carried out on wet and dry intact samples of Verzasca Gneiss at T = 300 and 500 °C, P c = 500 and 1030 MPa,...
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Veröffentlicht in: | Journal of structural geology 2007-01, Vol.29 (8), p.1282-1300 |
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Sprache: | eng |
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