Водосодержащие минералы в мантии Земли
https://doi.org/10.33623/MSU0579-9406-4-2025-64-5-3-26
Аннотация
Глубинные оболочки Земли отличаются различным содержанием воды. Основной механизм переноса воды из земной коры и Мирового океана в глубинные оболочки связан с процессами субдукции океанической литосферы. Мантийная переходная зона, благодаря способности накапливать воду номинально безводными минералами (вадслеитом и рингвудитом) представляет собой ее важнейший резервуар, особенно в сравнении с верхней мантией. Верхнемантийные перидотиты в составе погружаемых плит внутри переходной зоны могут сохранять H2O на больших глубинах в таких соединениях, как «алфавитные» DHMS фазы. Состав перидотита нижней мантии включает 80 масс. % Mg-перовскита (бриджманита), 15 масс. % ферропериклаза и 5 масс. % Ca-перовскита (дейвмаоита). Среди этих минералов наибольшее содержание воды допускается в Ca-перовските, за которым следуют Mg-перовскит и ферропериклаз. Учитывая огромную массу мантии Земли, даже минимальное количество воды, сосредоточенное в номинально безводных фазах, может в несколько раз превышать количество воды в современной гидросфере, несмотря на дегазацию мантии в результате вулканической деятельности, происходившей особенно интенсивно в первые 500 млн лет формирования планеты. Дана структурная характеристика минералов — возможных аккумуляторов воды в условиях глубинных геосфер.
Ключевые слова
При поддержке: Автор благодарен членам-корреспондентам РАН Ф.В. Каминскому и Н.Н. Еремину, профессорам А.Л. Перчуку и Н.В. Зубковой за советы и обсуждение этой работы. Исследование выполнено в рамках государственного задания МГУ имени М.В. Ломоносова.
Об авторе
Д. Ю. Пущаровский
Московский государственный университет имени М.В. Ломоносова
Россия
Россия
Пущаровский Дмитрий Юрьевич.
Москва
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Рецензия
Для цитирования:
Пущаровский Д.Ю. Водосодержащие минералы в мантии Земли. ВЕСТНИК МОСКОВСКОГО УНИВЕРСИТЕТА. СЕРИЯ 4. ГЕОЛОГИЯ. 2025;64(5):3-26. https://doi.org/10.33623/MSU0579-9406-4-2025-64-5-3-26
For citation:
Pushcharovsky D.Yu. The hydrated minerals in the Earth’s mantle. Moscow University Bulletin. Series 4. Geology. 2025;64(5):3-26. (In Russ.) https://doi.org/10.33623/MSU0579-9406-4-2025-64-5-3-26
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