Fluid Flux in Fractured Rock of the Alpine Fault Hanging-Wall Determined from Temperature Logs in the DFDP-2B Borehole, New Zealand-Reference-Cited by-同舟云学术

Fluid Flux in Fractured Rock of the Alpine Fault Hanging-Wall Determined from Temperature Logs in the DFDP-2B Borehole, New Zealand

Published:2018-08 Issue:8 Volume:19 Page:2631-2646
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Janku-Capova Lucie¹^ORCID,Sutherland Rupert¹^ORCID,Townend John¹^ORCID,Doan Mai-Linh²^ORCID,Massiot Cécile³^ORCID,Coussens Jamie⁴^ORCID,Célérier Bernard⁵

Affiliation:

1. School of Geography, Environment and Earth Sciences; Victoria University of Wellington; PO Box 600, Wellington New Zealand

2. Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, IFSTTAR, ISTerre, 38000 Grenoble, France

3. GNS Science; Lower Hutt Wellington New Zealand

4. Ocean and Earth Science; National Oceanography Centre Southampton, University of Southampton, European Way; Southampton, SO14 3ZH United Kingdom

5. Géosciences Montpellier; Université de Montpellier, CNRS; Montpellier France

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2017GC007317/fullpdf

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3. Fluid-flow along potentially active faults in crystalline rock;Barton;Geology,1995

4. Distribution of present-day vertical deformation across the Southern Alps, New Zealand, from 10 years of GPS data;Beavan;Geophysical Research Letters,2010

5. Influence of topographically driven convection on heat flow in the Swiss Alps: A model study;Bodri;Tectonophysics,1998

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