Genesis and Geodynamic Significance of Chromitites from the Fuchuan Ophiolite, Southern China, as Evidenced by Trace Element Fingerprints of Chromite, Olivine and Pyroxene
Author:
Affiliation:
1. Anhui Technical College of Industry and Economy Hefei 230051 China
2. Hefei University of Technology Hefei 230009 China
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14958
Reference71 articles.
1. Compositional variations of chromite and solid inclusions in ophiolitic chromitites from the southeastern Turkey: Implications for chromitite genesis
2. Anhui Bureau of Geology and Mineral Exploration 1995.Regional Geological Report of Shexian area Hefei Scale 1:500 000. Hefei: Anhui Bureau of Geology and Mineral Exploration Geological Report (in Chinese).
3. Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation
4. Origin of podiform chromitites
5. A study on the chemical composition of mineral inclusions in chromite from the Hegenshan ophiolite massif, Inner Mongolia, China;Bai W.J.;Acta Mineralogica Sinica,1993
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