摘要
康古尔塔格断裂带是东疆规模最大的一条汉断裂带，在泥盆系、石炭系中显示为韧性剪切带，具有剪切与挤压的交替作用，呈多期变形的特征，是黄山铜镍成矿带的导岩导矿构造。其次级韧性剪切带Ｆ８，Ｆ１１，Ｆ１２，，Ｆ９等为配岩配矿构造，而更低序次的韧性剪切带及其间沉积构造岩块中的早期褶皱或叠加褶皱是其直接的容岩容矿构造。本文着重探讨了黄山、香山和黄山东三个铜镍含矿基性超基性杂岩体的控岩控矿构造应力条件，并探讨了黄山铜镍成矿带构造控岩控矿模式。
Kangguertuge fault zone is the largest scale deep structure zone in eastern Xinjiang.It is showing as a Kangguermge ductile shear belt in Devonian and Carboniferou Systems.It'S moving characteristics are alternate shearing and compressing,and multiple deforming. The Kuangguertage ductile shear belt is the structure as passage ways for magma and ore fluid of Huangshan Cu-Ni metullogenic belt. It'S second-order ductile Shear belts F8,F11,F12 .F9 are the distributing rock and ore structures,and more low order ductile shear belts and early folds or superPOsed folds in sedimentary blocks all are direct-holding rock and host structures.This paper emphatically study controlling rock and ore tectonic stress conditions of Huangrhan,Xiangshan and east Huangshan three Cu-Ni ore bering mafic-ultramafic complexes,and discuss the structural controlling rock and ore model of Huangshan Cu-Ni metallogenic belt.
出处
《矿物岩石》
CAS
CSCD
1996年第1期86-93,共8页
Mineralogy and Petrology
关键词
铜矿床
镍矿床
成矿带构造
控岩模式
控矿模式
Cu-Ni metallogenic belt
ductile shear belt
tectonic stress structural controlling rockand ore model,Kuangguertage fault zone
