摘要
本文概述了陕西小秦岭地区金堆城──黄龙铺（钼）矿田区域地质构造基本特征及其与中生代含（钼）矿岩体之间的关系；重点探讨了成矿期燕山期地洼区正性单位，地穹有利构造部位对矿床控岩控矿的规律。
we, in this paper, generally described the basic geological. structure featrues in the molybdenum ore field geological region mainly in HUANG LONGPR the Jinduicheng of the small Qinling district, Shanxi Province, and their relationship with its molybdenum ore rock boby in the Mesozoic Era, the focus is to explore the positive elements of the depression during the mineralization and Yanshan epoch, and the law of the geodome advantageous structure positon towards the rock controlling and mineral controlling of the ore beds.
关键词
钼矿物
陕西
成矿地质构造
geodome structure, rock control and mineral control, structural delta region,metallogenic formation, mineralization epoch
