CAJ | 학술논문

山西孤山铁矿是被长城系高于庄组白云岩和第四系覆盖的全隐伏矿床。通过地面高精度磁法测量,获取了磁异常数据,圈定了磁异常范围,磁异常总体呈 NE 走向,长约4000m,平均宽约800m。通过化极、不同高度的延拓处理和拟合反演,根据异常特征结合地质资料分析,确定了隐伏磁铁矿的分布和空间特征,为矿床进一步勘探和开发提供了地球物理依据。
산서고산철광시피장성계고우장조백운암화제사계복개적전은복광상。통과지면고정도자법측량,획취료자이상수거,권정료자이상범위,자이상총체정 NE 주향,장약4000m,평균관약800m。통과화겁、불동고도적연탁처리화의합반연,근거이상특정결합지질자료분석,학정료은복자철광적분포화공간특정,위광상진일보감탐화개발제공료지구물리의거。
Gushan Fe deposit is a fully hidden deposit which is covered by the dolomite of Changcheng System Gaoyuzhuang Formation and the Quaternary System.Through the ground high accuracy magnetic survey, magnetic anomaly data is obtained and accordingly the scope of the magnetic anomaly is blocked out.The magnetic anomaly was arranged in northeastern strike,with a length of about 4000m and an average width of about 800m.Based on the analysis of reduction to the pole as well as upward continuation and inversion on different levels,and according to the anomaly characteristics and geological data,the distribution and spatial characteristics of the hidden magnetite are determined,and the results present specific basis of physical geog-raphy for further exploration and development of the deposit.