LU Shi-peng, Bao Kuan-le, Sun Jun-gang, Ding Xian-hua, QI Jing-jie
Abstract
新疆哈拉奇地区位于西南天山与塔里木盆地接触部位,属于航空磁法测量的边缘区,未开展过地面物探工作.此次开展地面高精度磁测工作,划分了6个区域磁异常区,圈定了3处次级高磁异常和1处局部高磁异常.推断区域磁异常由隐伏基性侵入岩、基底引起,次级高磁异常由构造引起,局部异常由矿体引起.磁异常解释为地质研究、寻找磁性矿产提供了参考依据.
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新疆哈拉奇地区位于西南天山与塔里木盆地接触部位,属于航空磁法测量的边缘区,未开展过地面物探工作.此次开展地面高精度磁测工作,划分了6个区域磁异常区,圈定了3处次级高磁异常和1处局部高磁异常.推断区域磁异常由隐伏基性侵入岩、基底引起,次级高磁异常由构造引起,局部异常由矿体引起.磁异常解释为地质研究、寻找磁性矿产提供了参考依据.
Key concepts: Geology, Magnetic anomaly, Anomaly (physics), Magnetic survey, Aeromagnetic survey, Geophysics, Seismology, Magnetic field