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卡乌留克塔格地区地质及磁异常特征
引用本文:郗国庆.卡乌留克塔格地区地质及磁异常特征[J].化工矿产地质,2011,33(2):108-113.
作者姓名:郗国庆
作者单位:中化地质矿山总局地质研究院,河北涿州,072754
摘    要:卡乌留克塔格C-12磁异常位于兴地大断裂南侧,航磁为低缓异常,地磁异常则极值较大.通过地面高精度磁法工作,确定了航磁异常在地面的具体位置及形态、范围及变化特征.根据磁异常的推断解释,C-12异常为超基性岩体引起.由此可见,磁法测量对寻找基性、超基性含铁磷岩体具有重要的意义.

关 键 词:磁异常  卡乌留克塔格

GEOLOGICAL AND MAGNETIC SIGNATURE OF KAWULIUKE TAG DISTRICT
Xi Guoqing.GEOLOGICAL AND MAGNETIC SIGNATURE OF KAWULIUKE TAG DISTRICT[J].Geology of Chemical Minerals,2011,33(2):108-113.
Authors:Xi Guoqing
Institution:Xi Guoqing Geological Institute of China Chemical Geology and Mine Bureau,Zhuozhou,Hebei,072754,China
Abstract:C-12 magnetic anomaly of Kawuliuke Tag district was located on the south of Xingdi fracture,the aeromagnetic survey result of which is lower but the geomagnetism anomaly has the higher extremum value.We identified the exact location,shape,scale and the variety characteristics of the aeromagnetic anomaly after finished the ground magnetic survey of high precision.We found that the C-12 anomaly was caused by ultrabasic rockbodies,all of which show that magnetic survey has significance for searching basic and ultrabasic ferriferous phosphorus bodies.
Keywords:magnetic anomaly  Kawuliuke Tag
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