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The document discusses carbonate reservoirs in the Kutai Basin region of East Kalimantan, Indonesia. It analyzes the distribution, depositional environments, and factors controlling the quality of carbonate reservoirs. Carbonate reservoirs range in age from Oligocene to Late Miocene and were deposited in shallow marine environments. However, the preservation of primary porosity is generally poor due to diagenetic processes such as calcite cement infilling.

Author

Iqbal

Language

EN