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Introduction Oceanic waves can carry charged ions dissolved in seawater, and electromagnetic fields can be induced by the dynamo interaction of ocean waves with the geomagnetic field. The ocean wave-induced electromagnetic fields can be observed at various locations, including the seafloor, sea surface, and, sometimes, even at satellite altitudes (Crews and Futterman, 1962; Cox et al., 1978; Minami, 2017).
Chao Su, Guoqing Ma, Cai Liu, Yunhe Liu and Bo Zhang* College of Geoexploration Science and Technology, Jilin University, Changchun, China In a sedimentary environment, the conventional one-dimensional (1D) inversion based on the horizontal layered model has difficulty restoring the resistivity distribution of the inclined strata when a coal seam has some dip angle or a small interval between layers.
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