Chromian spinel geochemistry as a petrogenetic indicator in the chromitites and peridotites of the Bajgan Complex, Western Makran
IntroductionEconomic chromite deposits are very common in ophiolite belts. These deposits usually occur in the uppermost horizons of the ophiolite mantle sequence or within the ultramafic cumulitic rocks at the base of the crustal sequence (González-Jiménez et al., 2014a; González-Jiménez et al., 20...
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| Principais autores: | , , |
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| פורמט: | Artigo |
| שפה: | Persa |
| יצא לאור: |
University of Isfahan
2025-06-01
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| סדרה: | پترولوژی |
| נושאים: | |
| גישה מקוונת: | https://ijp.ui.ac.ir/article_29577_e3efbbe00b63d835f73264302765d73a.pdf |
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