What can we learn from REE abundances in clinopyroxene and orthopyroxene in residual mantle peridotites?
Author:
Funder
Directorate for Geosciences
China Scholarship Council
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-021-01780-x.pdf
Reference66 articles.
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3. Baker MB, Stolper EM (1994) Determining the composition of high-pressure mantle melts using diamond aggregates. Geochim Cosmochim Acta 58:2811–2827
4. Bedini R, Bodinier JL (1999) Distribution of incompatible trace elements between the constituents of spinel peridotite xenoliths: ICP–MS data from the East African Rift. Geochim Cosmochim Acta 63:3883–3900
5. Bodinier J-L, Godard M (2014) Orogenic, ophiolitic, and abyssal peridotites. In: Carlson RW (ed) Treatise on geochemistry: the mantle and core, 2nd edn. Elsevier, New York, pp 103–167
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