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泥盆纪时,在阿尔泰山南缘拉张背景下,北西向区域性断裂和北北东向同生断裂的发育和复合,为火山喷发、潜火山岩分布和裂谷海水下渗循环创造了条件。伴随构造演化形成了两个构造-岩浆-成矿带。其中,一个成矿带是以与流纹-英安质火山活动有关的沉积岩型铅锌、(铁)多金属矿床(可可塔勒式)为特征,另一个成矿带是以与细碧-角斑质火山活动有关的火山岩型铜锌矿床(阿舍勒式)为特征。火山盆地、同生断裂和潜火山岩体顶部裂隙带控制了不同形式矿化。从裂谷边缘向中心,具有Fe→Pb-Zn,(Fe)-Cu-Pb-Zn→Cu-Zn矿化分布模式。
During the Devonian period, the development of the northwest trending faults and the NE-trending syngenetic faults in the background of the extension of the southern margin of the Altay Mountains created the conditions for volcanic eruptions, subvolcanic rock distribution and infiltration cycle of rift seawater. With the tectonic evolution formed two tectonic - magmatic - metallogenic belt. Among them, a metallogenic belt is characterized by sedimentary rock type Pb-Zn and (Fe) polymetallic deposits (cocoa Tale type) related to the rhyolite-British amphibious volcanic activity. Hornblende volcanic activity related to the volcanic type Cu-Zn deposit (Ascher type) is characterized. Volcanic basins, Tongsheng fault and the top rift zone of subvolcanic rock mass control different forms of mineralization. From the edge of the rift to the center, there are Fe → Pb-Zn, (Fe) -Cu-Pb-Zn → Cu-Zn mineralization distribution patterns.