FASIES KIPAS BAWAH LAUT PADA BATUAN BERUMUR PEREM-TRIAS, DAERAH KEKNENO, CEKUNGAN TIMOR

Authors

  • Asep Kurnia Permana Pusat Survei Geologi
  • A.H Prastian

DOI:

https://doi.org/10.33332/jgsm.geologi.v14i4.74

Abstract

Cekungan Timor termasuk kedalam kategori semi mature yang memiliki potensi hidrokarbon, namun kompleksitas kondisi geologi dan banyaknya konsep yang berbeda-beda merupakan salah satu penyebab stratigrafi di cekungan ini sulit dimengerti. Penelitian stratigrafi rinci untuk mengidentifikasi fasies dan sub fasies lingkungan pada batuan berumur Perem-Trias dilakukan di daerah Kekneno, Nenas, Cekungan Timor untuk memberikan pandangan baru mengenai stratigrafi, sedimentologi dan fasies lingkungan pengendapan pada batuan berumur Perem-Trias di cekungan ini. Hasil analisis litofasies menunjukkan bahwa batuan yang berumur Perem di daerah Kekneno diendapkan pada fasies lereng bagian bawah sampai atas (lower to upper slope facies), sedangkan batuan berumur Trias umumnya diendapkan sebagai fasies sistem kipas luar (outer fan system facies), fasies paparan luar samping lereng atas (outer shelf to upper slope facies), fasies sistem kipas tengah (middle fan system facies), dan fasies sistem kipas dalam (inner fan system facies). Endapan-endapan alur (channel) dan pematang (levee) pada batuan berumur Trias berpotensi menjadi target play hidrokarbon.


Kata Kunci: fasies, kipas bawah laut, batuan Perem-Trias, Cekungan Timor

Downloads

Download data is not yet available.

References

Audley-Charles, M.G., Carter, D.J., 1968. Paleogeographical significance of some aspects of Paleogene and Early Neogene Stratigraphy and tectonics of the Timor Sea region. Paleogeography, Paleoclimatology, Paleoecology, 11:247-264.

Bird, P.R and Cook, S.E., 1991. Permo-Trias Succession of the Kekneno Area, West Timor: Implication for Paleogeography and Basin Evolution. Journal of Southeast Asian Earth Sciences 6(3/4):359-371.

Bouma, A.H., 1962. Sedimentology of some flysch deposits. Amsterdam, Elsevier, 168 p.

Charlton, T.R., 2001. The Perm of Timor: stratigraphy, palaeontology and palaeogeography. Journal of Asian Earth Science 20 :719-774.

Charton.T.R.,2001. The Petroleum Potential of West Timor. Proocedings of the Indonesian Association 28,301-317, Indonesia.

Hamilton, W., 1979. Tectonics of the Indonesian Region. United States Geological Survey, p.1079.

King, P.R., Browne, G.H. and Slatt, R.M. 1994. Sequence architecture of exposed late Miocene basin floor fan and channel–levee complexes (Mount Messenger Formation), Taranaki Basin, New Zealand. In:Eds P. Weimer, A.H. Bouma and B.F. Perkins Submarine Fans and Turbidite Systems; Sequence Stratigraphy, Reservoir Architecture and Production Characteristics, Gulf of Mexico and International,pp. 177–192.

Nichols, G., 2009. Sedimentology and Stratigraphy Second Edition. Wiley-Blackwell by a John Wiley & Sons, Ltd, UK.

Permana, A.K., 2012. Laporan Akhir Penelitian Stratigrafi Cekungan Timor Kelompok Kerja Survei Dinamika Cekungan Tahun Anggaran 2012. Pusat Survei Geologi, Badan Geologi, Kementerian Energi Dan Sumber Daya Mineral, Bandung.

Sani, K., Jacobson, I., Sigit, R., 1995. The Thin-Skinned Thrust Structures of Timor. Proceedings of the Indonesian Petroleum Association 24 Annual Convention 24, 277-193, Indonesia.

Sawyer, R.K., Sani, K., Brown, S., 1993. Stratigraphy and Sedimentology of West Timor, Indonesia. Proccedings of the Indonesian Petroleum Association 22:1-20, Indonesia.

Shanmugam, G., 2005. Deep-Water Processes and Facies Models: Implications For Sandstone Petroleum Reservoirs. Department of Earth and Environmental Sciences The University of Texas, U.S.A.

Walker, R. G., dan James, N. P., 1992. Facies Model, Response to Sea Level Change. Geological Association of Canada, Kanada.

Downloads

Published

2013-11-19