Особенности эволюции химического состава фосфатов как отражение многофазного становления щелочно-карбонатитовой флюидо-эксплозивной системы Среднего Тимана

I. I. Golubeva, V. N. Filippov, A. S. Shuyskiy, I. N. Burtsev

Аннотация


В щелочно-карбонатитовую флюидо-эксплозивную систему на Среднем Тимане входят карбонатиты, карбонатизированные флюидо-экспозивные дайки и фенитизированные терригено-карбонатные породы рифея. Во всех породах кристаллизуются фосфаты, представленные монацитом и апатитом. Химический состав минералов свидетельствует о многофазности становления данной системы и едином источнике флюидов, участвовавших в ее формировании.

Ключевые слова


монацит; апатит; флюидо-эксплозивная система; Средний Тиман

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Литература


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DOI: http://dx.doi.org/10.17072/psu.geol.22.3.201

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