摘要
在综合研究前人大量资料的基础上,综合地物化遥等信息,探讨隆林地区下一步找矿方向,取得以下成果:研究区的主干断裂为岭皓断裂,前三叠纪具多期次同沉积活动特点,明确了下一步找矿方向。其本身不含矿或仅为矿化。其旁测的次一级断层破碎带、节理、裂隙及劈理给来自深源的矿质提供了有利的容矿空间,形成了小仁金矿、菜家湾金矿、以及锑、汞、铅锌矿等内生矿产。
On the basis of comprehensive research on a large number of predecessors, comprehensive information on geodesic and remote information, explore the next prospecting direction in Longlin area, and achieve the following results:the main fault in the study area is Lingling fault, and the first Triassic has multiple phases. With the characteristics of sedimentary activities, the next prospecting direction is clarified. It does not contain minerals or is only mineralized. The sub-level fault fracture zone, joints, fissures and cleavage provided by the side-by-side test provide favorable ore-bearing space for the minerals from the deep source, forming the Xiaoren Gold Mine, the Caijiawan Gold Mine, and the strontium,mercury and lead. Endogenous minerals such as zinc ore.
引文
[1]赵金科,张文佑.广西地质地层概要[M].科学出版社.1959.
[2]贵州省区域地质调查队.1:20万安龙幅区域地质调查报告.1980年.