Геохимия хромового рудогенеза

R. G. Iblaminov

Аннотация


Формирование месторождений хромовых руд обусловлено геохимическими параметрами хрома, приводящими к его накоплению в остаточном мантийном расплаве, а в экзогенных условиях – на восстановительном барьере в составе волконскоита. Геохимия определяет минеральный состав хромшпинелевых руд и их технологические свойства и применение.

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Литература


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DOI: http://dx.doi.org/10.17072/psu.geol.22.4.364

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