Partitioning of Ti, Al, P, and Cr between olivine and a tholeiitic basaltic melt: Insights on olivine zoning patterns and cation substitution reactions under variable cooling rate conditions-Reference-Cited by-同舟云学术

Partitioning of Ti, Al, P, and Cr between olivine and a tholeiitic basaltic melt: Insights on olivine zoning patterns and cation substitution reactions under variable cooling rate conditions

Published:2022-07 Issue: Volume:601 Page:120870
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Lang Sarah,Mollo Silvio,France Lydéric,Misiti Valeria,Nazzari Manuela

Funder

INSU

CNRS

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference77 articles.

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2. Partitioning coefficients between olivine and silicate melts;Bédard;Lithos,2005

3. XANES measurements of Cr valence in olivine and their applications to planetary basalts;Bell;Am. Mineral.,2014

4. Titanium substitution mechanisms in forsterite;Berry;Chem. Geol.,2007

5. Electron paramagnetic resonance and ENDOR studies of Cr3+-Al3+ pairs in forsterite;Bershov;Phys. Chem. Miner.,1983

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