Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.
岩形于具有基性火山作用的活动大陆边缘滨海-浅海环境。经过宙的区域高角闪岩相变质作用,形岩系。
Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.
岩形于具有基性火山作用的活动大陆边缘滨海-浅海环境。经过宙的区域高角闪岩相变质作用,形岩系。
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