Effects of changes in metallic mineral to time domain induced polarization (TDIP) response on physical modeling fieldscale

Manganese prospecting using time domain induced polarisation (TDIP), case study: Karangnunggal district, Tasikmalaya regency

“…One of the geophysical methods that can map the earth's subsurface is the time domain induced polarization (TDIP) method. The parameter acquired is chargeability; it initially describes the ability to store a material's electrical energy and is sensitive to a conductive material content [10,[13][14][15][16]. A high chargeability value indicates the presence of metallic mineral zones in the study area [16][17][18][19].…”

“…A high chargeability value indicates the presence of metallic mineral zones in the study area [16][17][18][19]. Many studies have implemented the induced polarization method for minerals prospecting [14][15][16][17][18][19][20][21][22]. Even the electrical resistivity methods only have also been applied [23,24].…”

“…Even the electrical resistivity methods only have also been applied [23,24]. Some focused on manganese minerals with similar results in interpreting from chargeabiliy data [14][15][16][17][18][19][20]. But, some combine it with other methods, such as resistivity [16][17][18][19] or electromagnetics [20].…”