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...

وصف كامل

التفاصيل البيبلوغرافية
الحاوية / القاعدة:	پترولوژی
المؤلفون الرئيسيون:	Leila Vahedi, Morteza Delavari, Emilio Saccani
التنسيق:	مقال
اللغة:	الفارسية
منشور في:	University of Isfahan 2025-06-01
الموضوعات:	podiform chromite high-cr and high-al chromite peridotite western makran iran
الوصول للمادة أونلاين:	https://ijp.ui.ac.ir/article_29577_e3efbbe00b63d835f73264302765d73a.pdf

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