The capacity of hydrous fluids to transport and fractionate incompatible elements and metals within the Earth's mantle-Reference-Cited by-同舟云学术

The capacity of hydrous fluids to transport and fractionate incompatible elements and metals within the Earth's mantle

Published:2014-06 Issue:6 Volume:15 Page:2241-2253
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Adam John¹,Locmelis Marek²,Afonso Juan Carlos¹,Rushmer Tracy¹,Fiorentini Marco L.²

Affiliation:

1. Australian Research Council Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Department of Earth and Planetary Sciences; Macquarie University; New South Wales Australia

2. Centre for Exploration Targeting, Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, School of Earth and Environment; The University of Western Australia; Crawley, Western Australia Australia

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference53 articles.

1. The geochemistry and experimental petrology of sodic alkaline basalts from Oatlands, Tasmania;Adam;J. Petrol.,1990

2. Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: Experimental results and the investigation of controls on partitioning behaviour;Adam;Contrib. Mineral. Petrol.,2006

3. Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 2. Tasmanian Cainozoic basalts and the origins of intraplate basaltic magmas;Adam;Contrib. Mineral. Petrol.,2011

4. Trace element partitioning between aqueous fluids, silicate melts and minerals;Adam;Eur. J. Mineral.,1997

5. The survival of mantle geochemical heterogeneities

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