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新疆库鲁克塔格阔克苏地区基性岩墙群由一系列北西向延伸,间距大致相等的辉绿岩岩墙组成。岩墙群侵入于前寒武纪变质岩和花岗岩中,边界平直,局部具有追踪张裂的特征。为提供该区构造演化的地质年代学及岩石地球化学依据,笔者
The basic dyke swarm in the Kuruktag-Gokkesu region of Xinjiang consists of a series of diabase dikes extending roughly north-west and equally spaced. The dyke swarms intrude into the Precambrian metamorphic rocks and granites, and the boundaries are straight and locally tracing the faults. In order to provide geologic chronology and geochemical basis for the tectonic evolution of the area, I author