Pressure-dependent compatibility of iron in garnet: Insights into the origin of ferropicritic melt-Reference-Cited by-同舟云学术

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Pressure-dependent compatibility of iron in garnet: Insights into the origin of ferropicritic melt

Published:2017-01 Issue: Volume:197 Page:356-377
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Zhang JunBo,Liu YongSheng,Ling WenLi,Gao Shan

Funder

National Nature Science Foundation of China

Ministry of Education of China

State Administration of Foreign Expert Affairs of China

MOST

State Key Laboratory of Geological Processes and Mineral Resources

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference158 articles.

1. Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. Experimental results and the investigation of controls on partitioning behaviour;Adam;Contrib. Mineral. Petrol.,2006

2. Solid–liquid iron partitioning in Earth’s deep mantle;Andrault;Nature,2012

3. Coupled 186Os–187Os enrichments in the Earth’s mantle – core–mantle interaction or recycling of ferromanganese crusts and nodules?;Baker;Earth Planet. Sci. Lett.,2004

4. Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions;Barth;Precambr. Res.,2002

5. The effect of sodium and titanium on crystal-melt partitioning of trace elements;Bennett;Geochim. Cosmochim. Acta,2004

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