Ambari, Wardahrose Dhifa
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MIDDLE MIOCENE TO HOLOCENE GEOLOGICAL HISTORY AND POTENTIAL OF BABAKAN JAWA AREAS, MAJALENGKA DISTRICT OF WEST JAVA-INDONESIA Ambari, Wardahrose Dhifa; Sunardi, Edy; Ilmi, Nisa Nurul
Journal of Geological Sciences and Applied Geology Vol 9, No 1 (2026): Journal of Geological Sciences and Applied Geology
Publisher : Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v9i1.69279

Abstract

Geological mapping activities were conducted in the Sidamukti, Babakan Jawa, Cibodas areas and surroundings, Majalengka District, West Java Province. The main objective of this research is to determine the geomorphological characteristics, lithology, geological structures, and geological potential in the research area. The methods used include field observations, laboratory analysis, interpretation of topographic maps and satellite imagery, as well as structural analysis using stereonet. The research results show that the geomorphology of the study area was formed by the interaction of endogenic forces (tectonic and volcanic) and exogenic forces (weathering and erosion), resulting in five main geomorphological units. The stratigraphy of the area consists of five rock units composed of claystone units from the Middle Miocene to Holocene alluvial deposits. The developed geological structures indicate the influence of extensional stress with a strike-slip component that forms normal faults and reverse faults trending northwest–southeast. The geological potential of the area includes resources such as andesite stone, sand, and gravel, as well as the geotourism potential of Taman Gunung Batu Karang. On the other hand, steep hilly areas with weathered lithology show vulnerability to mass movements, making them landslide-prone areas. The results of this mapping are expected to serve as a basis for sustainable natural resource management and geological disaster mitigation.
SOURCE ROCK CHARACTERISTICS AND THERMAL MATURITY IN JAMBI SUB-BASIN, SOUTH SUMATRA BASIN Ambari, Wardahrose Dhifa; Ilmi, Nisa Nurul; Sunardi, Edy
Journal of Geological Sciences and Applied Geology Vol 9, No 2 (2026): Journal of Geological Sciences and Applied Geology
Publisher : Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v9i2.70656

Abstract

The Jambi Sub-Basin, located within the South Sumatra Basin, represents one of the prospective hydrocarbon-bearing areas in Indonesia due to the presence of organic-rich syn-rift and post-rift sedimentary sequences and a well-developed petroleum system. This study aims to evaluate source rock characteristics and hydrocarbon generation potential of several stratigraphic interval in the Jambi Sub-Basin using Total Organic Carbon (TOC) and Rock-Eval Pyrolysis data obtained from fourteen wells in the study area. The analyses were conducted to assess the quantity, quality, and thermal maturity of organic matter within the source rocks. The results indicate that the Lower Talang Akar Formation (LTAF) and Upper Talang Akar Formation (UTAF) could become the most prospective source rock intervals, characterized by moderate to excellent TOC values with S2 values ranging from poor to excellent generative potential. Organic matter is primarily composed of type II-III kerogen, indicating dominant terrestrial organic matter input deposited in fluvia-deltaic to marginal lacustrine environment, with the capability to generate mixed gas and oil hydrocarbons. Hydrogen Index (HI) values range from 14 to 561 mg HC/ g TOC, reflecting variable organic matter quality and depositional conditions across the basin. Thermal maturity parameters, including Tmax and vitrinite reflectance, indicate maturity levels ranging from immature to post mature stages. The Talang Akar intervals generally show higher maturity levels associated with deeper burial and prolonged thermal evolution, suggesting active hydrocarbon generation, particularly gas generation in the deeper areas. The integration of organic richness, kerogen type, and maturity distribution suggests that the LTAF represents the principal gas-prone source rock within the study area, while several intervals still has their oil-generation potential. This study could provide an integrated organic geochemical framework for evaluating source rock distribution in the Jambi Sub-Basin and contribute to the improvement of future hydrocarbon exploration strategies in the South Sumatra Basin.Keyword: source rock, Rock-Eval Pyrolysis, Talang Akar Formation, Thermal Maturity, South Sumatra Basin