Local partial melting of the lower crust triggered by hydration through melt-rock interaction: an example from Fiordland, New Zealand-Reference-Cited by-同舟云学术

Local partial melting of the lower crust triggered by hydration through melt-rock interaction: an example from Fiordland, New Zealand

Published:2016-11-18 Issue:2 Volume:35 Page:213-230
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J. Metamorph. Geol.

Author:

Stuart C. A.¹^ORCID,Daczko N. R.¹,Piazolo S.¹

Affiliation:

1. ARC Centre of Excellence for Core to Crust Fluid Systems and GEMOC; Department of Earth and Planetary Sciences; Macquarie University; Sydney NSW 2109 Australia

Funder

ARC Future Fellowship

Discovery Project

ARC LIEF

DEST Systemic Infrastructure Grants

Macquarie University and Industry

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12229/fullpdf

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3. Chemical diffusion of major components in granitic liquids: implications for the rates of homogenization of crustal melts;Acosta-Vigil;Lithos,2012

4. The capacity of hydrous fluids to transport and fractionate incompatible elements and metals within the Earth's mantle;Adam;Geochemistry, Geophysics, Geosystems,2014

5. Fluid flow in the deep crust;Ague;Treatise on Geochemistry,2003

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