Reactivation of normal faults as high-angle reverse faults due to low frictional strength: Experimental data from the Moonlight Fault Zone, New Zealand-Reference-Cited by-同舟云学术

Reactivation of normal faults as high-angle reverse faults due to low frictional strength: Experimental data from the Moonlight Fault Zone, New Zealand

Published:2017-12 Issue: Volume:105 Page:34-43
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Smith S.A.F.^ORCID,Tesei T.,Scott J.M.,Collettini C.

Funder

Marsden Fund Council

Royal Society of New Zealand

Publisher

Elsevier BV

Subject

Geology

Reference63 articles.

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3. The effect of mineralogy and effective normal stress on frictional strength of sheet silicates;Behnsen;J. Struct. Geol.,2012

4. On the nucleation of non-Andersonian faults along phyllosilicate-rich mylonite belts;Bistacchi,2012

5. Frictional-viscous flow of simulated fault gouge caused by the combined effects of phyllosilicates and pressure solution;Bos;Tectonophysics,2000

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