Fluid migration in the mantle wedge: Influence of mineral grain size and mantle compaction-Reference-Cited by-同舟云学术

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Fluid migration in the mantle wedge: Influence of mineral grain size and mantle compaction

Published:2017-08 Issue:8 Volume:122 Page:6247-6268
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Cerpa Nestor G.¹²^ORCID,Wada Ikuko¹^ORCID,Wilson Cian R.³^ORCID

Affiliation:

1. Department of Earth Sciences; University of Minnesota, Twin Cities; Minneapolis Minnesota USA

2. Now at Department of Earth Sciences; University of Oxford; Oxford UK

3. Department of Terrestrial Magnetism; Carnegie Institute for Science; Washington District of Columbia USA

Funder

University of Minnesota

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JB014046/fullpdf

Reference60 articles.

1. Overriding plate thinning in subduction zones: Localized convection induced by slab dehydration;Arcay;Geochem. Geophys. Geosyst.,2006

2. Viscosity of fluids in subduction zones;Audétat;Science,2004

3. Paleowattmeters: A scaling relation for dynamically recrystallized grain size;Austin;Geology,2007

4. Implications of grain size evolution on the seismic structure of the oceanic upper mantle;Behn;Earth Planet. Sci. Lett.,2009

5. Mechanical and thermodynamic constraints on fluid distribution in partial melts;Bulau;J. Geophys. Res.,1979

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