摘要
新疆东部的康古尔塔格断裂带不是板块俯冲带,而是地体的一条边界断裂带。其演化历史可分为三个主要阶段:深断裂活动阶段、韧性剪切活动阶段和断块活动阶段,并相应控制了阿齐山-黄山复合地体的形成与发展,还直接控制了黄山-镜儿泉地区铜镍含矿镁铁超镁铁杂岩体的空间展布与形态特征。
The geological and geophyscal data have proved that Kangguertage fault zone is an impor-tant fault zone in the eastern Xinjiang. It is not a plate subducted zone but is only a terrane boundaryfault zone. It's evolutional history can be divided into three main phases: deep fracture action, ductileShear deformation and fault block action. It controls not only the formation and development of Aqis-han-Huangshan composite terrane, but also directly the distribution and shape feature of the Cu-Ni orebearing mafic-ultramafic complex in Huangshan-Jingerquan area.
关键词
新疆
康古尔塔格
断裂带
地质
the eastern Xinjiang
Kangguertage fault zone
ductile shear zone
composite terrane
Cu-Ni ore bearing mafic-ultramafic complex
