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.
原岩形成于具有基性火的活
大陆边缘滨海-浅海环境。经过太古宙的区域高角闪岩相
质
,形成孔兹岩系。