Fracturing, fluid-rock interaction and mineralisation during the seismic cycle along the Alpine Fault-Reference-Cited by-同舟云学术

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Fracturing, fluid-rock interaction and mineralisation during the seismic cycle along the Alpine Fault

Published:2017-10 Issue: Volume:103 Page:151-166
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Williams Jack N.^ORCID,Toy Virginia G.,Smith Steven A.F.,Boulton Carolyn

Funder

GNS Science

Victoria University of Wellington

University of Otago

University of Auckland

University of Canterbury

Deutsche Forschungsgemeinschaft

University of Bremen

Natural Environment Research Council

University of Liverpool

Royal Society of New Zealand

NERC

Publisher

Elsevier BV

Subject

Geology

Reference117 articles.

1. Permeability and seismic velocity and their anisotropy across the Alpine Fault, New Zealand: an insight from laboratory measurements on core from the Deep Fault Drilling Project phase 1 (DFDP-1);Allen;J. Geophys. Res. Solid Earth,2017

2. New insights to temperature and pressure beneath the central Southern Alps, New Zealand;Allis;N. Z. J. Geol. Geophys.,1995

3. Rupture dynamics with energy loss outside the slip zone;Andrews;J. Geophys. Res. Solid Earth,2005

4. Hydrothermal alteration in an exhumed crustal fault zone: testing geochemical mobility in the Caleta Coloso Fault, Atacama fault system, Northern Chile;Arancibia;Tectonophysics,2014

5. Oscillatory zoning and trace element incorporation in hydrothermal minerals: insights from calcite growth experiments;Barker;Geofluids,2011

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4. Along-strike architectural variability of an exhumed crustal-scale seismogenic fault (Bolfin Fault Zone, Atacama Fault System, Chile);Journal of Structural Geology;2022-12

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