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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。
The Kanggutage fault zone is the largest Han fault zone in East Xinjiang. It shows ductile shear zone in the Devonian and Carboniferous rocks and has the alternation of shear and compression with multi-period deformation. Is Huangshan copper-nickel metallogenic belt guide rock structure. The secondary ductile shear zones F8, F11, F12, F9 and so on are of the ore-bearing structure, while the lower-order ductile shear zones and the early folds or overlying folds in the interlaminar sedimentary rocks are their direct Rock capacity mine structure. This paper focuses on the tectonically controlled tectono-tectonic conditions of the three copper-nickel ore-bearing base ultramafic complexes in Huangshan, Xiangshan and Huangshan East and discusses the tectonically controlled rock control model for the Huangshan copper-nickel metallogenic belt.