An Early Garnet Redox‐Filter as an Additive Oxidizer in Lower Continental Arc Crust Traced Through Fe Isotopes

Author:

Li Qi‐Wei123ORCID,Nebel‐Jacobsen Yona2,Zhao Jun‐Hong1,Nebel Oliver2,Richter Marianne2,Cawood Peter A.2ORCID,Wang Qiang345ORCID

Affiliation:

1. State Key Laboratory of Geological Processes and Mineral Resources School of Earth Sciences China University of Geosciences Wuhan China

2. School of Earth, Atmosphere and Environment Monash University Clayton VIC Australia

3. State Key Laboratory of Isotope Geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

4. CAS Center for Excellence in Deep Earth Science Guangzhou China

5. College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

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

Reference125 articles.

1. Igneous garnet and amphibole fractionation in the roots of island arcs: experimental constraints on andesitic liquids

2. Compositions of anhydrous and hydrous melts coexisting with plagioclase, augite, and olivine or low‐Ca pyroxene from 1 atm to 8 kbar: Application to the Aleutian volcanic center of Atka;Baker D. R.;American Mineralogist,1987

3. Oxygen fugacity controls in the Earth's upper mantle

4. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe

5. Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas

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