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Report on Geological Survey of Central Kalimantan: Consolidated Report
The integrated surveys have been conducted in the Central Kalimantan, aiming to make clear geology, stratigraphical sequences, igneous activities, geological structures and mineralizations and to investigate possibilities of natural resources based on the study of relationship between geology and mineral deposits. As a results of the geological surveys conducted from several phases in the area of about 2.000 KM2, geology, stratigraphical sequences, igneous activities, geological structures and mineralizations in the mapped area were made much more clear. There are two stages of mineralization in the area, one is an earlier mineralization forming mineralized zones in metamorphic rocks of the basement and in tonalites of the late Permian and the close of Jurassic Periods. Another is a later mineralization related to plutonic or hypabyssal igneous activities and volcanisms during periods from the close of Cretaceous to Tertiary. Three anomalous areas were found; mineralized zones of porphyry copper-type areas, copper-bearing pyritic ore veins and gold-lead-zinc ore veins. Target areas are suggested to be investigated further. The continuation and expansion of the survey were also recommended.
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