Abstract
Electromagnetic exploration using the CSAMT method was conducted to reveal the distribution of saltwater and freshwater beneath the Nakano-shima Island, Oki-Dozen, which is located on a continental shelf. For better interpreting the resistivity structure in the Island, rock samples obtained from the Island were used to measure bulk resistivities as a function of the salinity of pore water. Existence of inferred fault which formed depression structure is suggested by previous studies. Contrast of resistivity distribution found from measurement points which across the inferred fault was interpreted as difference of geological structure bounded by the fault. The resistivity distributions in depression showed the higher resistivity zone from surface to about －100m elevation, the lower resistivity zone in between －100 and －200m elevation, the higher resistivity zone below, and the lower resistivity zone further below, i.e., the existence of four distinct resistivity zones. Each zone was interpreted, as descending order, modern fresh groundwater, groundwater with higher salinity, fresh groundwater recharged in colder climate, and groundwater with higher salinity.
