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

用
活动大陆边缘
海-浅海环境。经过太

区域高角闪岩相变质
用,形成孔兹岩系。
、未受造山地震等因素影响
之境
不得不相互竞争,这对生命来
非常艰难,我们失去了大
95% 
究人员认为,当南极洲



