摘要
白云岩是冶炼金属镁的一种重要矿产资源。本文以赋存于上寒武统—下奥陶统三山子组中的山西隰县岭上地区白云岩矿为研究对象,通过对区域地质背景、矿区地质、矿体地质、矿石质量等特征的总结,提出了本区白云岩矿的找矿标志、岭上白云岩矿床成因——岭上白云岩矿床为沉积型浅海相沉积型准同生+准同生后白云岩的组合成因矿床;三山子组一段(∈_(3)s^(1))层位,可作为山西隰县黄土镇岭上一带白云岩矿的找矿标志。
Dolomite is an important mineral resource for smelting magnesium.This paper deals with regional geological background,geology of the mining area and ore bodies and ore quality of the dolomite ore deposit occurring in Upper Cambrian-Lower Ordovician Sanshanzi Formation in Lingshang area,Xianxian county,Shanxi province and puts forward prospecting marks and genesis of the dolomite deposit.The deposit is a marine sedimentary penesyngenetic + post-penesyngenetic dolomite deposit.The first member(∈_3s^(1)) of the formation is the prospecting mark of such dolomite deposit.
作者
韩效斌
弓晨
王勇
郎学聪
李沛龙
游立辉
HAN Xiaobin;GONG Chen;WANG Yong;LANG Xuecong;LI Peilong;YOU Lihui(The Third Geological Exploration Institute,China Metallurgical Geology Bureau,Taiyuan 030032,Shanxi,China)
出处
《地质找矿论丛》
CAS
2024年第2期186-191,共6页
Contributions to Geology and Mineral Resources Research
关键词
冶镁白云岩
白云岩矿
地质特征
矿床成因
岭上地区
隰县
山西省
Dolomite for smelting Mg
geological characteristics
genesis of dolomite deposit
Lingshang area
Xixian county
Shanxi province
