论文部分内容阅读
罗卜岭大型铜(钼)矿床位于福建省上杭县紫金山矿田的东部,区内断裂构造发育,岩浆侵入活动强烈,成矿条件优越,矿床的形成与燕山晚期花岗闪长斑岩体有关,也受到多期次构造的影响。本文通过对罗卜岭铜钼矿床含矿裂隙空间分布规律、铜钼元素空间水平分带和深部斑岩隐伏矿体及其与斑岩体和区域构造空间关系的综
The large-scale copper (molybdenum) ore deposit in Loebling is located in the east of Zijinshan orefield in Shanghang County, Fujian Province. The fault structure is developed and the magmatic intrusion activity is strong and the metallogenic conditions are superior. The formation of the deposit coincides with the late Yanshan granodiorite porphyry Body related, but also by the impact of multi-phase structure. Based on the spatial distribution of the ore-bearing fractures in the Luobuling copper-molybdenum deposit, spatial division of copper and molybdenum elements, and the comprehensive relationship between the buried porphyry and the porphyry bodies and regional tectonics