综合物探方法在川东高陡断褶带隐伏断层勘探中的应用研究

四川盆地东部地区位于华蓥山与七曜山之间,经历多期次复杂的构造叠加和改造,形成了高陡构造带及断层,高陡构造带内探测分辨隐伏断层是地球物理勘探的难点。本文通过重、磁、电探测方法的正反演模拟成果得出高陡断褶带隐伏断层能够被探测识别,并结合利用重、磁、电综合物探方法在川东高陡断褶带探测隐伏断层的实际应用效果,总结了隐伏断层的异常形态和异常特征。同时总结了野外数据采集干扰压制的试验成果,断层破碎带异常的正演反演处理手段。本文为川东地区地质勘查工作提供参考依据和经验积累。

The application of integrated geophysical prospecting to the exploration of buried faults in the high and steep fault-fold zone in eastern Sichuan

The eastern region of Sichuan basin is located between Huaying Mountain and Qiyaodan Mountain. After multiple periods of complex structural superposition and transformation, high and steep tectonic belts and faults were formed. It is difficult to detect and distinguish hidden faults in the high and steep tectonic belts in geophysical exploration. Based on the forward and inverse simulation results of gravity, magnetic and electric detection methods, the authors have reached the conclusion that buried faults in high and steep fault folds can be detected and recognized. Combined with the practical application effect of gravity, magnetic and electric integrated geophysical prospecting methods in high and steep fault folds in eastern Sichuan, the authors summarized the abnormal morphology and abnormal characteristics of buried faults . At the same time, the experimental results of field data acquisition interference suppression and the forward inversion processing method of fault fracture zone anomalies were also summarized. The results obtained by the authors provide a reference basis and experience accumulation for geological exploration in eastern Sichuan.