PETROGRAFI KARAKTERISTIK BATUPASIR FORMASI GAMPING WUNGKAL IMPLIKASI UNTUK PROVENAN, DIAGENESIS, DAN PROSES PENGENDAPAN, FORMASI GAMPING WUNGKAL, KECAMATAN BAYAT, KABUPATEN KLATEN, PROVINSI JAWA TENGAH
DOI:
https://doi.org/10.34151/technoscientia.v12i1.1844Keywords:
Compaction, Diagenesis, Mesodiagenesis, ProvenanAbstract
Gamping Wungkal Formation, middle Eocene to Upper Eocene, which consists of sandstones, sandy marl, claystone and limestone which are the problems of provenance rock, diagenesis and its deposition process. Retrieval of stratigraphic data to determine the deposition process which is divided into several facies and determine its depositional environment, petrographic observations to determine the type of rock, provenance, tectonic settings. Interpretation of tectonic settings of sandstones Gamping Wungkal Formations on QFL diagram plots include recycled orogens, foreland uplift sub-zones while the plot in the QmFLt diagram of the provenance rock is the same as the QFL diagram, which is recycled orogen, sub-zone foreland uplift, rock model from recycled orogen foreland uplift sub-zone. The sandstone diagenesis of the Gamping Wungkal Formation in the study area is included in the mesodiagenesis stage where the compaction or burial process still dominates, the depositional environment in the study area is an area formed in the transitional environment or intertidal flat (Middle tidal flat) and subtidal (Lower tidal flat).
References
Burley, D. S., dan Worden, H. R., (editor), 2003, Sandstone Diagenesis: Recent and Ancient, Reprint Series, vol. 4, The International Association of Sedimentologist, Wiley-Blackwell, England.
Dickinson, W. R., dan Suczek, C. A., 1979, Plate Tectonics and Sandstone Compositions, The American Association of Petroleum Geologists Bulletin, vol. 63., No. 12, p. 2164-2182.
Folk, R. L., 1974, Petrology of Sedimentary Rocks, Hemphill Publishing Company, Austin.
Husein, S., Novian, I. M., 2014, Geology Excursion to Bayat, Central Java, Guide Book, Santos (Sampang) Pty Ltd and Departement of Geological Engineering UGM.
Pettijohn, F. J., 1975, Sedimentary Rocks, 3rd ed., Harper & Row, New York.
Prasetyadi, C., 2007, Evolusi Tektonik Paleogen Jawa Bagian Timur, Disertasi, Program Studi Teknik Geologi, Institut Teknologi Bandung, tidak dipublikasikan.
Purnomo J. dan Purwoko, 1994, Kerangka Tektonik dan Stratigrafi Pulau Jawa Secara Regional dan Kaitannya dengan Potensi Hidrokarbon, Prosiding Geology and Geoteknik Pulau Jawa, Seminar Jurusan Teknik Geologi Fakultas Teknik UGM, Yogyakarta.
Smyth, H., Hall, R., Hamilton, J., dan Kinny, P., 2005, East Java: Cenozoic Basins, Volcanoes, and Ancient Basement, Proceedings 30th Indonesian Petroleum Association Annual Convention and Exhibition, Jakarta.
Sudarno, 1997, Kendali Tektonik Terhadap Pembentukan Struktur Pada Batuan Paleogen dan Neogen di Pegunungan Selatan, Daerah Istimewa Yogyakarta Dan Sekitarnya, Tesis, Program Studi Teknik Geologi, Institut Teknologi Bandung, tidak dipublikasikan.
Tortosa, A., Palomares, M., dan Arribas, J., 1991, Quartz Grain Types in
Holocene Deposits from The Spanish Central System: Some Problems in
Provenance Analysis, In: Developments in Sedimentary Provenance Studies, Geol. Soc. London Spec. Pub., vol. 57, p. 47-54.
