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
火山作用的活动大陆边缘
海-浅海环境。经过太古宙的

角闪岩相变质作用,形成孔兹岩系。

如果她能看得更远一点,看到
和凯普莱
完全是由造礁珊瑚沉积形




员遇到了蒙


