浆;
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.
形成于具有基性火
活动大陆边缘滨海-浅海环境。经过太古宙区域高角闪相变
，形成孔兹系。
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.
形成于具有基性火活动大陆边缘滨海-浅海环境。经过太古宙区域高角闪相变，形成孔兹系。
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