Diagenesis Study of Jatiluhur Formation at Cipamingkis River, Bogor Regency, West Java, Indonesia
DOI:
https://doi.org/10.25299/jgeet.2021.6.4.7646Keywords:
Diagenesis features, Diagenesis history, Jatiluhur Formation, Petrography, XRD, SEMAbstract
Diagenesis studies in the Jatiluhur Formation are still relatively new, especially in the Cipamingkis River. This research can provide information in the form of components and characteristics of sandstone in the Jatiluhur Formation which can be used as a basis for further research or useful information in the oil and gas industry. Knowledge of diagenetic could be one of the factors that affect in raservoir quality, espesially in sandstone. In this study, data collection was carried out through surface mapping, which is 55 rock samples were obtained from stratigraphic measuring section with a path length of ±2 Km in the Cipamingkis River. The data is in the form of information on sedimentarry structure, textures and composition. There were 23 sandstone and 2 limestone samples which were then subjected to petrographic analysis, X-ray diffraction (XRD) and scanning electron microscopy (SEM). The results of study are several features of diagenesis were found including compaction that works in the form of point contact, long contact, concavo-convex contact and suture contact and dominated by mechanical compaction, while in limestone there is a brittle fracture feature in bioclasts. The cement found in the form of calcite cement, quartz and clay minerals that the form of kaolinite, smectite and illite, while the limestone is in the form of blocky and fibrous to bleded which is filled with calcite minerals. Dissolution occurs in the minerals of quartz, feldspar, and mica. The mineral replacement that is commonly found occurs in quartz and feldspar minerals. In limestone, there is an intergranular micritization. The dominant type of porosity found was interparticle with an average of 10.4% found between 3 – 23%. The history of diagenesis that occurs in rocks in the Jatiluhur Formation begins with the initial deposition of eogenesis, followed by burial mesogenesis and ends with telogenesis which reveals rocks on the surface.
Downloads
References
Abdurrokhim. (2017). Stratigrafi Sikuen Formasi Jatiluhur di Cekungan Bogor, Jawa Barat. Bulletin of Scientific Contribution, 15(2), 167–172.
Abdurrokhim, & Ito, M. (2013). The role of slump scars in slope channel initiation: A case study from the Miocene Jatiluhur Formation in the Bogor Trough, west java. Journal of Asian Earth Sciences, 73, 68–86.
Berner, R. A. (1980). Early Diagenesis: A Theoretical Approach. Princeton Series in Geochemistry, Princeton University Press.
Bjørlykke, K., & Egeberg, P. K. (1993). Quartz cementation in sedimentary basins. American Association of Petroleum Geologists Bulletin, 77, 1536–1548.
Boggs Jr, S. (2013). Principles of Sedimentology and Stratigraphy, Edisi ke-5. Prentice Hall.
Boles, J. R., & Franks, S. . (1979). Clay diagenesis in Wilcox sandstones of southwest Texas: implications of smectite diagenesis on sandstone cementation. Journal of Sedimentary Petrology, 49, 55–70.
Burns, R. G., & Burns, V. . (1977). Chapter 7 Mineralogy. In Marine Manganese Deposits; Glasby, G.P., Ed. Elsevier.
Chima, P., Baiyegunhi, C., Liu, K., & Gwavava, O. (2018). Diagenesis and rock properties of sandstones from the Stormberg Group, Karoo Supergroup in the Eastern Cape Province of South Africa. Open Geosciences, 10(1), 740–771.
Curtis, C. D. (1977). Geochemistry: Sedimentary geochemistry: Environments and processes dominated by involvement of an aqueous phase. Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 286(1336), 353–372.
Giles, M. R., Indrelid, S. L., Beynon, G. V., & Amthor, J. (2000). The origin of large-scale quartz cementation: evidence from large datasets and coupled heat-fluid mass transport modelling. In: Quartz Cementation in Sandstones (Eds R.H. Worden & S. Morad). Spec. Publs Int. Assoc. Sediment. Blackwell Science, Oxford, 29, 21–38.
Hall, R., & Morley, C. . (2004). Sundaland basins. In: Clift, P., Wang, P., Kuhnt, W., Hayes, D.E. (Eds.), Continent–Ocean Interactions within the East Asian Marginal Seas. Geophysical Monograph 149. American Geophysical Union, 55–85.
López-Quirós, A., Escutia, C., & Sánchez-Navas, A. (2019). Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation. Sci Rep 9, 13580.
Milliken, K. . (2003). Diagenesis. In: Encyclopedia of Sediments and Sedimentary Rocks (Ed. Middleton, G.V.). Kluwer Academic Publishers.
Morad, S., Ketzer, J. M., & De Ros, L. . (2000). Spatial and temporal distribution of diagenetic alterations in siliciclastic rocks: implications for mass transfer in sedimentary basins. Sedimentology, 47. Millenium Reviews, 95–120.
Rahman, M. A., Astuti, T. R. P., & Supriyanto. (2019). Petrography and Scanning Electron Microscope Study for Provenanve and Tectonic Setting Implication of Middle-Late Miocene Sandstone of Jatiluhur Formation, Bogor Trough, West Java. 2nd International Congress on Earth Sciences.
Rahman, M. J. J., Mccann, T., Abdullah, R., & Yeasmin, R. (2011). Sandstone diagenesis of the Neogene Surma Group from the Shahbazpur Gas Field, Southern Bengal Basin, Bangladesh. Austrian J. Earth Sci, 104, 114–126.
Ramseyer, K., Boles, J. R., & Lichtner, P. . (1992). Authigenic K–NH4–feldspar in sandstones: a fingerprint of the diagenesis of organic matter. Journal of Sedimentary Petrology, 62, 349–356.
Schmidt, V., & Macdonald, D. . (1979). The role of secondary porosity in the course of sandstone diagenesis. In: Aspects of Diagenesis (Eds P.A. Scholle & P.R. Schuldger). Soc. Econ. Paleont. Miner. Spec. Publ., Tulsa. OK, 29, 175–207.
Sudjatmiko. (1972). Peta Geologi Regional Lembar Cianjur, Jawa Barat Skala 1:100.000. Pusat penelitian dan pengembangan geologi.
Waltham, D., Hall, R., Smyth, H. R., & Ebinger, C. J. (2008). Basin formation by volcanic arc loading. The Geological Society of America Special Paper 436, 11–26.
Waugh, B. (1971). Formation of quartz overgrowths in the Penrith Sandstone (Lower Permian) of northwest England as revealed by scanning electron microscopy. Sedimentology, 17, 309–320.
Wilkinson, M., Milliken, K. L., & Haszeldine, R. . (2001). Systematic destruction of K-feldspar in deeply buried rift and passove margin sandstones. Journal of the Geological Society, London, 158, 675–683.
Worden, R. H., & Burley, S. D. (2003). Sandstone diagenesis: The evolution of sand to stone. Sandstone Diagenesis, 1–44.
Downloads
Published
Issue
Section
License
Copyright @2019. This is an open-access article distributed under the terms of the Creative Commons Attribution-ShareAlike 4.0 International License which permits unrestricted use, distribution, and reproduction in any medium. Copyrights of all materials published in JGEET are freely available without charge to users or / institution. Users are allowed to read, download, copy, distribute, search, or link to full-text articles in this journal without asking by giving appropriate credit, provide a link to the license, and indicate if changes were made. All of the remix, transform, or build upon the material must distribute the contributions under the same license as the original.
