Effective global mixing of the highly siderophile elements into Earth’s mantle inferred from oceanic abyssal peridotites
Author:
Funder
University of California, San Diego
National Science Foundation
NSF EAR
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference108 articles.
1. In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle;Alard;Nature,2005
2. Non-chondritic distribution of the highly siderophile elements in mantle sulphides;Alard;Nature,2000
3. Geodynamic mixing in the mesosphere boundary layer and the origin of oceanic islands;Allègre;Geophys. Res. Lett.,1985
4. Distribution and processing of highly siderophile elements in cratonic mantle lithosphere;Aulbach;Rev. Mineral. Geochem.,2016
5. Seawater-peridotite interactions: First insights from ODP Leg 209, MAR 15°N;Bach;Geochem. Geophys. Geosyst.,2004
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