For one month from June to July in 1970, ground geophysical surveys, induced polarization (I.P.) and self-potential (S.P.) methods, were carried out in the area of Mamut Mine by the present writers under the contract with Overseas Mineral Resources Development Co., Ltd.
In general, the I.P. and the S.P. methods can not distinguish economic sulphides, e⋅g., chalcopyrite from pyrite, but the I.P. anomaly can indicates the percentage of the total sulphides. These methods are especially applicable for the area rich in chalcopyrite and pyrite.
These surveys were carried out for determining the volume of the known ore body and prospecting new mineralized zones of the porphyry copper-type deposits at Mamut.
The volume and dip of the ore deposit of the Mamut-2 mine were deduced trom the detailed I.P. data. In addition, adaptability of the S.P. method to the disseminated sulphides deposits with intensely oxidized crust was confirmed. This environment can be expected in a hot and highly humid area with a shallow ground-water level.
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