PROVENANCE ANALYSIS OF THE RAMPONG FORMATION SANDSTONE IN THE KETUKAH AREA, GAYO LUES, ACEH

Dewi Sartika; Dina Gunarsih; Luthfi Ahmad; Akmal Muhni; Lia Fitria Rahmatillah; Muhammad Ridha Adhari

doi:10.29303/ipr.v7i1.261

PROVENANCE ANALYSIS OF THE RAMPONG FORMATION SANDSTONE IN THE KETUKAH AREA, GAYO LUES, ACEH

Authors

Dewi Sartika , Dina Gunarsih , Luthfi Ahmad , Akmal Muhni , Lia Fitria Rahmatillah , Muhammad Ridha Adhari

DOI:

10.29303/ipr.v7i1.261

Published:

2023-11-07

Issue:

Vol. 7 No. 1 (2024)

Keywords:

Rampong Formation, provenance, petrography, sandstone

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Sartika, D., Gunarsih, D., Ahmad, L., Muhni, A., Rahmatillah, L. F., & Adhari, M. R. (2023). PROVENANCE ANALYSIS OF THE RAMPONG FORMATION SANDSTONE IN THE KETUKAH AREA, GAYO LUES, ACEH. Indonesian Physical Review, 7(1), 39–51. https://doi.org/10.29303/ipr.v7i1.261

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Abstract

The research location is in Ketukah, Gayo Lues Aceh, which is composed of the Late Oligocene to Early Miocene Rampong Formation. Lithology includes sandstones, conglomerates, and mudstones. The study aims to determine the origin of the sandstones in the Rampong Formation. Provenance studies are beneficial in providing information for oil and gas exploration. The analysis is critical for understanding the sediment transport channel, the overall depositional pattern of the basin, and predicting the location of sand bodies in the basin. Because the Rampong Formation is located in the North Sumatra Basin, the availability of provenance information is useful in efforts to search for oil and gas potential in the future. In this research, we restrict the study to the provenance, which includes the tectonic setting, origin rock, and paleoclimate where these sandstones originate. The methods are geological mapping and petrographic analysis. In petrographic analysis, we use JMicrovision to calculate mineral composition. The results showed that the sandstones of the Rampong Formation are arenite sandstones, especially sub-arkosic and sub-lith arenite. They originate from a tectonic setting known as a recycled orogen, related to the subduction of Eurasia and the Indo-Australian plates. The sandstones were formed from granite that had undergone low metamorphism in the Late Cretaceous to the Eocene period. In addition, the paleoclimate is humid.

References

N.R. Cameron, J. D. Bennett, D. McC Bridge, M. C. Clarke, A. Djunuddin, S. A. Ghazali, H. Harahap, D. H. Jeffery, W. Kartawa, W. Keats, H. Ngabito, N. M. Rocks, and S. J. Thompson. “Geological Map Of The Takengon Quadrangle, Sumatera.” Bandung: Geological Survey Institute, 2007.

R. W. Bemmelen, “The Geology of Indonesia,” New York: U.S. Government Printing Office, 1949.

F.J. Pettijohn, P.E. Potter, R. Siever, “Sand and Sandstone,” New York: Springer, 1987.

W.R. Dickinson and C. Suzcek, ” Plate tectonic and sandstone compositions,” The American Associations of Petroleum Geologists Bulletin, vol. 63, pp. 2164-2182, 1979.

Z. Zhang and H. Wang, “Comprehensive provenance analysis and its applications to Eocene Clastic Rocks in the Huimin Depression, Bohai Bay Basin, China.” Journal Minerals, vol. 9, 2019.

G. S. Nugraha, E. Sunardi, I. Haryanto, B. G. Adhiperdana, R. Fakhruddin, R. Fitriany, D. Gunarsih, “ Facies analysis, biostratigraphy, and provenance of the late Neogene Seulimeum Formation, Northwest Aceh basin, Sumatra (Indonesia).” Journal Heliyon, vol 9, 2023.

A. J. Barber, M. J. Crow, and J. S. Milsom, “Sumatra: Geology, Resources and Tectonic Evolution,” London: Geological Society, 2005.

M. S. Rosid, N. N. Tullailah, and R. A. Wibowo, “Identification of potential hydrocarbon traps in area X pre-tertiary sediments of the North Sumatra basin using gravity and seismic data,” Journal UNNES, vol 10, 2020.

R. L. Folk, “Petrology of Sedimentary Rocks,” Texas: Hemphill Publishing Company, 1979.

A. Basu, S.W. Young, L. J. Suttner, W. C. James, G. H. Mack, “Re-evaluation of the use of undulatory extinction and polycrystallinity in detrital quartz for provenance interpretation.” Journal of Sedimentary Research, vol. 45, pp. 871-882, 1975.

W. R. Dickinson, “Interpreting provenance relations from detrital modes of

sandstones.” In: Provenance of Arenites, Dordrecht: Springer, 1985, pp. 333-361.

M. E. Tucker, “Sedimentary Petrology.” United Kingdom: Blackwell Science, 2001.

W. S. MacKenzie, A. E. Adams, and K. H. Brodie. “Rocks and Minerals in Thin Section.” London: CRC Press.

S. Boggs, “Petrology of Sedimentary Rocks.” New York: Cambridge University Press, 2009.

M. L. Larrea, S. M. Castro, E. A. Bjerg, “A software solution for point counting. Petrographic thin section analysis as a case study,” Arabian Journal Geoscience, 2013.

F.J. Pettijohn, “Sedimentary rocks,” New York: Harper & Row, 1975.

W. R. Dickinson, L. S. Beard, G. R. Brakenridge, J. L. Erjavec, R. C. Ferguson, K. F. Inman, R. A. Knepp, F. A. Lindberg, P. T. Ryberg, “Provenance of North American Phanerozoic sandstones in relation to tectonic setting,” Geological Society of American Bulletin, vol. 94, p. 222-235, 1983.

S. A. Nelson, “Petrology Sandstone and Conglomerate,” New Orleans: Tulane University, 2007.

A. Tortosa, M. Palomares, dan J. Arribas, “Quartz grain types in Holocene deposits from the Spanish Central System: some problems in provenance analysis,” Geological Society, vol 57, pp. 47-54, 1991.

B. Ahmer dan S. K. Muhammad, “Petrography and provenance of sandstone and studies of shale of Kuldana formation, Kalamula and Khursheedabad area, Kahuta,” Azad Kashmir Earth Sci. Malaysia (ESMY), vol. 1 (1), pp. 21-31, 2017.

W. L. Brown dan I. Parsons, “Feldspars in Igneous Rocks,” In Parsons, I. (eds) Feldspars and their Reactions. NATO ASI Series, vol 421. Dordrecht: Springer, 1994.

Author Biography

Akmal Muhni, Universitas Syiah Kuala

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PROVENANCE ANALYSIS OF THE RAMPONG FORMATION SANDSTONE IN THE KETUKAH AREA, GAYO LUES, ACEH

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Akmal Muhni, Universitas Syiah Kuala

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