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西藏玉龙斑岩铜(钼)矿带以斑岩铜矿闻名于世,玉龙铜矿则是世界级的超大型斑岩铜矿。玉龙铜(钼)矿带位于青泥洞复式背斜的西翼,其中觉拥(温泉)断裂延展远、切割深度大,对区域地质发展史起着重要的控制作用。在这样的地质背景下,玉龙铜(钼)矿外围存在大量的斑岩体,已发现几十个斑岩体,较大的有15个,但是其中含矿斑岩屈指可数。正文将重点放在讨论玉龙铜矿的地质概况和玉龙铜(钼)矿的南段(纳加扎地区)和北段(甘龙拉地区)的斑岩体含矿性与找矿潜力。
The Yulong porphyry copper (molybdenum) ore belt in Tibet is famous for its porphyry copper deposits, while the Yulong copper deposit is a world-class super-large porphyry copper deposit. The Yulong copper (molybdenum) ore belt is located in the west wing of the Qingni-dong multi-anticline, where the fault zone of Jue Yong (hot spring) extends far and has a large depth of cut and plays an important role in controlling the history of regional geological development. Under such geological background, there are a large number of porphyry bodies outside the Yulong copper (molybdenum) mine. There are dozens of porphyry bodies, 15 of which are large, but there are a few porphyry ore-bearing porphyries. The text will focus on discussing the geology of Yulong Copper Mine and the porphyry ore-bearing and prospecting potential in the southern section (Nagarza region) and the northern section (甘龙拉 region) of the Yulong copper (molybdenum) mine.