Time-dependent permeability evolution in compacting volcanic fracture systems and implications for gas overpressure-Reference-Cited by-同舟云学术

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Time-dependent permeability evolution in compacting volcanic fracture systems and implications for gas overpressure

Published:2017-06 Issue: Volume:339 Page:81-97
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Farquharson Jamie I.^ORCID,Wadsworth Fabian B.,Heap Michael J.,Baud Patrick

Funder

University of Strasbourg

CNRS-INSU

Agence Nationale de la Recherche

Explosive Volcanism in the Earth System: Experimental Insights; EVOKES

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference87 articles.

1. Acid alteration in the fumarolic environment of Usu Volcano, Hokkaido, Japan;Africano;J. Volcanol. Geotherm. Res.,2000

2. Element variations in rhyolitic magma resulting from gas transport;Berlo;Geochim. Cosmochim. Acta,2013

3. Explosive origin of silicic lava: textural and δD-H2O evidence for pyroclastic degassing during rhyolite effusion;Castro;Earth Planet. Sci. Lett.,2014

4. Rapid laccolith intrusion driven by explosive volcanic eruption;Castro;Nat. Commun.,2016

5. The role of melt-fracture degassing in defusing explosive rhyolite eruptions at Volcán Chaitén;Castro;Earth Planet. Sci. Lett.,2012

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