KONTROL STRUKTUR PADA POLA “ZIG-ZAG” ALIRAN SUNGAI KAYAN DI DAERAH PESO, KALIMANTAN TIMUR

Authors

  • Baharuddin Baharuddin Pusat Survei Geologi
  • Joko Wahyudiono

DOI:

https://doi.org/10.33332/jgsm.geologi.v17i3.288

Abstract

Peso Area is situated at the downstream of Kayan River, East Kalimantan. The area is generally occupied by a flysch-type deposit of Cretaceous Rajang-Embaluh Group. The unit is unconformably overlain by the Tertiary Sediments and is intruded by the Tertiary-Quaternary magmatics. Based on interpretation of landsat imagery, lineament features which represent faults can be traced outside the studied area. Based on landsat imagery data and result of joints, fault and fold analyses, it can be concluded that the zig-zag pattern of the Kayan River at Peso area is closely related to major faults movements. These faults are generally trending NE- SW and NW-SE.

 

Keywords : structural control, zig-zag patterns, Kayan River

Downloads

Download data is not yet available.

References

Anderson, E.M., 1951. The Dynamic of Faulting and Dyke Formation with application to Britain. Oliver and nd Boyd, Edinburg, London, 2 Edition, Revised.

Bachri, S., (dalam persiapan). Peta Interpretasi citra Landsat daerah Lembar Long Bia skala 1:250.000. Pusat Survei Geologi.

Haile, N.S ., Mc Elhinny, M.W & Mc Dougall, I., 1977. Paleomagnetic data and radiometric ages from the Cretaceous of West Kalimantan (Borneo), and their significance in interpreting regional structure. Journal Geological Society of London 133:133-144.

Hamilton, W., 1979. Tectonics of the Indonesian region. United States Geological Survey, Professional Paper, 1078.

Heryanto, R and H.Z. Abidin., 1995. Peta Geologi Lembar Long Bia, Kalimantan Timur (Peta Kompilasi) Sekala 1:250.000. Pusat Penelitian dan Pengembangan Geologi, Bandung.

Hutchison, C.S., 1988. Stratigraphic- Tectonic Model for Eastern Borneo, Geological Society Malaysia, Bulletin 22:135-151.

Hutchison, C.S., 1996. 'The Rajang accretionary prism' and 'Lupar Line' problem of Borneo. In Hall, R & Blundell,D. (eds). Tectonic Evolution of Southeast Asia. Geological Society Special Publication 106:247-261.

Moss, S.J., A.Carter., S.Baker., A.J. Hurford., 1998. A Late Oligocene tectono-volcanic event in East Kalimantan and the implications for tectonics and sedimentation in Borneo. Journal of the Geological Society.

Pieters, P.E ., Trail, D.S. & Supriatna, S., 1987. Correlation of Early Tertiary rocks across Kalimantan. Proceedings Indonesian Petroleum Association 16th annual convention: 291- 306.

Rickard, M.J., 1972. Fault Classification - Discussion. Geological Society American Bulletin:2545-2546. Simanjuntak, T.O., 2004. Tektonika, Pusat Penelitian dan Pengembangan Geologi, Bandung. Publikasi khusus 13:216.

Suryono, N., 1986. Tegasan Terputar dan Pembentukan Struktur Penyerta, Bulletin Teknologi Mineral UPN “Veteran†Yogyakarta 68:44-49.

Tanean, H., Paterson, D.W., & Mac Endharto., 1996. Source Provenance Interpretation of Kutai Basin Sandstones and the Implications for the Tectono-Stratigraphic evolution of Kalimantan. th Proceedings IPA, 25 Silver Anniversary Convention.

Vogt, E.T, & Flower, M.F.J., 1989. Genesis of the Kinabalu (Sabah) granitoid at a subduction- collision junction. Contributions to Mineralogy and Petrology103:493-509.

Downloads

Published

2007-06-30

Issue

Vol. 17 No. 3 (2007): Jurnal Sumber Daya Geologi

Section

Article

License

Authors who publish articles in Jurnal Geologi dan Sumberdaya Mineral (JGSM.Geologi) agree to the following terms:

  1. Authors retain copyright of the article and grant the journal right of first publication with the work simultaneously licensed under a CC-BY-NC or The Creative Commons Attribution–ShareAlike License.
  2. Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgment of its initial publication in this journal.
  3. Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access)