БУНДЕЛКХАНДСКИЙ, АРАВАЛЛИ И ДХАРВАРСКИЙ КРАТОНЫ ИНДИЙСКОГО ЩИТА: СРАВНИТЕЛЬНЫЙ АНАЛИЗ ИСТОРИИ РАЗВИТИЯ ЗЕМНОЙ КОРЫ В АРХЕЕ И ПОЛОЖЕНИЕ В СТРУКТУРЕ СУПЕРКОНТИНЕНТА КЕНОРЛЕНД
Аннотация
выделяется Бунделкхандский. В мезоархее новая континентальная кора формировалась здесь в ходе субдукционно-аккреционных процессов, в то время как на других кратонах отмечается влияние лишь мантийных плюмов. В неоархее на всех рассматриваемых кратонах отмечены проявления субдукционных и аккреционных геодинамических процессов. Рассматриваемые кратоны в мезо-неоархее входи-
ли в состав суперконтинента Кенорленд в качестве самостоятельных фрагментов и не образовывали единый блок.
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