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新疆喀默什特地区隐伏断裂高精度磁测解释
引用本文:鲍宽乐,闫金华,王庆同,李晓阳,鲁世朋,丁宪华. 新疆喀默什特地区隐伏断裂高精度磁测解释[J]. 中国区域地质, 2014, 0(1): 92-98
作者姓名:鲍宽乐  闫金华  王庆同  李晓阳  鲁世朋  丁宪华
作者单位:[1]中国人民武装警察部队黄金第七支队,山东烟台264004 [2]中国地质大学北京,北京100083
基金项目:中国地质调查局项目(编号:1212011120495、1212011220661)致谢:感谢武警黄金第七支队刘晓煌博士和吴怀志工程师在论文分析处理中在算法方面的指导.
摘    要:喀默什特南部戈壁覆盖区存在东西向正磁异常带,长约11km,在进行高精度磁法测量后推测为基性或超基性物质反磁化的反映。为了给出正磁异常带合理的解释,沿异常带垂直方向布设1:10000剖面,通过离散小波分解对剖面磁测数据进行精细化处理,得到不同深度范围内异常的分布。结合欧拉反褶积运算、归一化总梯度处理及空间域解析延拓进一步判断异常特征,发现该异常主要由断裂引起,为塔什纳拉他乌推覆体所引起的断裂在喀默什特南部的延伸段。

关 键 词:离散小波分解  欧拉反褶积  断裂  高磁异常

The high-precision magnetic survey explanation of concealed faults in Kamoshite area of Xinjiang.
BAO Kuan-le,YAN Jin-hua,WANG Qing-tong,LI Xiao-yang,LU Shi-peng,DING Xian-hua. The high-precision magnetic survey explanation of concealed faults in Kamoshite area of Xinjiang.[J]. Regional Geology of China, 2014, 0(1): 92-98
Authors:BAO Kuan-le  YAN Jin-hua  WANG Qing-tong  LI Xiao-yang  LU Shi-peng  DING Xian-hua
Affiliation:1. The 7th Gold Detachment of Chinese Armed Police Force, Yantai 264004, Shandong, China; 2. China University of Geosciences (Beijing), Beijing 100085, China
Abstract:There are widespread Quaternary overburdens in the south of Kamoshite, where there exists a EW-trending positive mag- netic anomaly belt about llkm long, which is supposed to be the reflection of basic or ultrabasic material reversed magnetization. In order to give a reasonable explanation, the authors arranged 1 : 10000 profiles to trace the strike of the anomaly. Through the fine dis- crete wavelet processing, the anomalies distributions at different depths were detected. Combined with Euler Deconvolution opera- tion and normalized total gradient domain processing, it is found that the anomaly is mainly caused by fault, which is the extension of the fault caused by Tash Narayan nappe in Kamoshite.
Keywords:DWT  Euler Deconvohition  fault  magnetic anomalies
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