Serpentinite-derived slab fluids control the oxidation state of the subarc mantle
Open Access
- 26 November 2021
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science Advances
- Vol. 7 (48)
Abstract
Incorporation of variable amounts of oxidizing slab fluids leads to globally heterogeneous oxidation state of the subarc mantle.Keywords
This publication has 69 references indexed in Scilit:
- Pressure–temperature estimates of the lizardite/antigorite transition in high pressure serpentinitesLithos, 2013
- The mean composition of ocean ridge basaltsGeochemistry, Geophysics, Geosystems, 2013
- Multiple mantle plume components involved in the petrogenesis of subduction‐related lavas from the northern termination of the Tonga Arc and northern Lau Basin: Evidence from the geochemistry of arc and backarc submarine volcanicsGeochemistry, Geophysics, Geosystems, 2007
- Distinct regional differences in crustal thickness along the axis of the Mariana Trough, inferred from gravity anomaliesGeochemistry, Geophysics, Geosystems, 2006
- Stable isotope compositions of serpentinite seamounts in the Mariana forearc: Serpentinization processes, fluid sources and sulfur metasomatismEarth and Planetary Science Letters, 2006
- Composition of the depleted mantleGeochemistry, Geophysics, Geosystems, 2004
- Two isotopically distinct fluid components involved in the Mariana arc: Evidence from Nb/B ratios and B, Sr, Nd, and Pb isotope systematicsGeology, 1999
- The boron systematics of intraplate lavas: Implications for crust and mantle evolutionGeochimica et Cosmochimica Acta, 1996
- Boron isotope systematics of marine sedimentsEarth and Planetary Science Letters, 1993
- Oxygen fugacity controls in the Earth's upper mantleNature, 1990