Slip and stress in block-in-matrix shear zones: 1. microstructure and mineralogy of a serpentine-filled dilational jog-Reference-Cited by-同舟云学术

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Slip and stress in block-in-matrix shear zones: 1. microstructure and mineralogy of a serpentine-filled dilational jog

Published:2024-09 Issue: Volume:186 Page:105220
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Smith Steven A.F.^ORCID,Tarling Matthew S.,Negrini Marianne,Allan Samantha J.,Ellis Susan^ORCID,Palmer Marshall,Viti Cecilia,Reid Malcolm R.^ORCID

Funder

Royal Society of New Zealand Marsden Fund

Publisher

Elsevier BV

Reference75 articles.

1. The subduction plate interface: rock record and mechanical coupling (from long to short timescales);Agard;Lithos,2018

2. A microstructural study of a “crack-seal” type serpentine vein using SEM and TEM techniques;Andreani;Eur. J. Mineral,2004

3. Development of schistosity by dissolution-crystallization in a Californian serpentinite gouge;Andreani;J. Struct. Geol.,2005

4. Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. Alps);Angiboust;Lithos,2011

5. Microchemical evidence for episodic growth of antitaxial veins during fracture-controlled fluid flow;Barker;Earth Planet Sci. Lett.,2006

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