With the development of geophysical exploration methods to fine exploration, it is found that the deviation of induced electromotive force between the edge of observation area and the central point in the wireframe is 15% ~ 25%, which can not be ignored compared with some anomalies caused by geological targets, such as collapse columns hundreds of meters deep, small water-conducting faults and metal deposits thousands of meters deep (Shi Xianxin et al., 2009). For the case of non-central point, the integration is complicated, which can not be directly converted into polynomial form, let alone Fourier transform, which is one of the main reasons why the interpretation technology of transient electromagnetic method with large loop source can not be improved. Therefore, the theoretical formula of large fixed source loop is introduced into the central loop device, and the two are unified to form a trend; On this basis, the research of apparent resistivity algorithm has become the focus of current research.
The responses of non-central point field and central point field of transient electromagnetic field of large loop source are compared and discussed. It is considered that kernel functions have similar functional forms and properties, so the components of non-central points can also be expressed as polynomial forms similar to the vertical components of central points. The definition of apparent resistivity is completed by undetermined coefficient method. The model test shows that the method is feasible and the result is reliable. This technology has detected two mines in Shannan region of Tibet, such as Pan 'an and Nuri (Xue Guoqiang et al., 2065438)