Carbonatite Versus Silicate Melt Metasomatism Impacts Grain Scale 87 Sr/ 86 Sr and 143 Nd/ 144 Nd Heterogeneity in Polynesian Mantle Peridotite Xenoliths-Reference-Cited by-同舟云学术

Carbonatite Versus Silicate Melt Metasomatism Impacts Grain Scale 87 Sr/ 86 Sr and 143 Nd/ 144 Nd Heterogeneity in Polynesian Mantle Peridotite Xenoliths

Published:2021-09 Issue:9 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Byerly Benjamin L.¹²^ORCID,Jackson M. G.¹^ORCID,Bizimis M.³^ORCID

Affiliation:

1. Isotope Geochemistry Facility—Center for Mantle Zoology Department of Earth Science University of California Santa Barbara CA USA

2. Thermo Fisher Scientific Waltham MA USA

3. School of the Earth, Ocean and Environment University of South Carolina Columbia SC USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009749

Reference83 articles.

1. Extreme isotopic heterogeneity in Samoan clinopyroxenes constrains sediment recycling

2. Quantifying trace element disequilibria in mantle xenoliths and abyssal peridotites

3. In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle

4. Metasomatism and Hydration of the Oceanic Lithosphere: a Case Study of Peridotite Xenoliths from Samoa

5. Distribution of incompatible trace elements between the constituents of spinel peridotite xenoliths: ICP-MS data from the East African rift

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