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<http://digilib.unila.ac.id/id/eprint/56652> <http://purl.org/dc/terms/title> "IDENTIFIKASI ZONA PROSPEK RESERVOIR MIGAS DAN GAS \r\nBIOGENIK MENGGUNAKAN DATA LOG, PETROFISIKA DAN \r\nGEOKIMIA PADA LAPANGAN “MN” CEKUNGAN NIAS SUMATERA \r\nUTARA"^^<http://www.w3.org/2001/XMLSchema#string> .
<http://digilib.unila.ac.id/id/eprint/56652> <http://purl.org/ontology/bibo/abstract> "The fore-arc basin has been become a target of reservoir searching for a long time \r\nbased on previous expert studies, where the indications of Late-Miocene carbonate \r\nage that could act as a hydrocarbon reservoir was found. ‘MN’ Field located in the \r\nNias Basin, one of the fore-arc basin located in West of Sumatera. As the object of \r\nthis study, it is hoped that the hydrocarbon reservoir in the fore-arc basin is expected \r\nto be discovered and to identify the characteristics of rocks that potential to become \r\nhydrocarbon reservoirs. Geochemical data becomes supporting data regarding the \r\npresence of gases that are identified as biogenic gases because of the content of \r\nmethane as the main composition. Identification of the existence of reservoir zones \r\nand source rock is done by qualitative interpretation of log data from the L-1, P-1, \r\nS-1, T-1 and UB-1 Well. Then, the petrophysical parameters are analyzed in the \r\nform of shale volume (Vsh), effective porosity, resistivity water (Rw), and water \r\nsaturation (Sw) to determine the type of reservoir’s fluid. After knowing the \r\npetrophysical parameters value, distribution area correlation of reservoir and source \r\nrock can be made in the study area. The results of the interpretation indicated that \r\nthe presence of biogenic gas was detected in S-1 and P-1 Well on limestone \r\nlithology with Late Miocene age. Biogenic gas in the ‘MN’ Field has PHIE value \r\ncharacteristics around 17,0 – 32,1 % and Sw value is 39,9 % - 61,3 %.\r\nKeywords: biogenic gas, hydrocarbon reservoir, immature source rock, limestone, \r\nLate Miocene\r\n\r\n\r\nThe fore-arc basin has been become a target of reservoir searching for a long time \r\nbased on previous expert studies, where the indications of Late-Miocene carbonate \r\nage that could act as a hydrocarbon reservoir was found. ‘MN’ Field located in the \r\nNias Basin, one of the fore-arc basin located in West of Sumatera. As the object of \r\nthis study, it is hoped that the hydrocarbon reservoir in the fore-arc basin is expected \r\nto be discovered and to identify the characteristics of rocks that potential to become \r\nhydrocarbon reservoirs. Geochemical data becomes supporting data regarding the \r\npresence of gases that are identified as biogenic gases because of the content of \r\nmethane as the main composition. Identification of the existence of reservoir zones \r\nand source rock is done by qualitative interpretation of log data from the L-1, P-1, \r\nS-1, T-1 and UB-1 Well. Then, the petrophysical parameters are analyzed in the \r\nform of shale volume (Vsh), effective porosity, resistivity water (Rw), and water \r\nsaturation (Sw) to determine the type of reservoir’s fluid. After knowing the \r\npetrophysical parameters value, distribution area correlation of reservoir and source \r\nrock can be made in the study area. The results of the interpretation indicated that \r\nthe presence of biogenic gas was detected in S-1 and P-1 Well on limestone \r\nlithology with Late Miocene age. Biogenic gas in the ‘MN’ Field has PHIE value \r\ncharacteristics around 17,0 – 32,1 % and Sw value is 39,9 % - 61,3 %.\r\nKeywords: biogenic gas, hydrocarbon reservoir, immature source rock, limestone, \r\nLate Miocene"^^<http://www.w3.org/2001/XMLSchema#string> .
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