Fault analysis to Determine Deformation History of Kubang Pasu Formation at South of UniMAP Stadium Hill, Ulu Pauh, Perlis, Malaysia

  • Adi Suryadi Universitas Islam Riau

Abstract

The Kubang Pasu Formation at South of UniMap Stadium Hill has suffered deformation that produced fault with various types and orientations. First deformation (ST1) is southeast – northwest were resulted normal, reverse, dextral and sinistral fault. At station 32, Reverse fault (N940E/480) from ST1 was cut by reverse fault (N480E/400) result of second deformation (ST2). Another cross cutting fault found at station 108, third deformation (ST3) with stress direction from northeast – southwest that produced reverse fault with strike direction N1340E and 680 of dip angle was cutting the reverse fault (N870E/660) from second deformation. The youngest deformation (ST4) has stress from east – west. At station 110, normal fault (N900E/300) is representing the youngest deformation was cutting the reverse fault (N1540E/520) from third deformation.

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References

[1] Gobbett, D. J. 1973. Upper Paleozoic. in. Gobbett, D. J. & Hutchison, C. S. (Edt). Geology of the Malay Peninsular: 61-95. New York: John Wiley & Sons, Inc.
[2] Jones, C.R. 1981. The geology and mineral resources of Perlis, north Kedah, and Langkawi Island. Geological Survey Malaysia District Memoir 17: 67-84.

[3] Zaiton Haron & Basir Jasin. 1999. Implication of the Bok Bak Fault movements on the structure and lithostratigraphy of the Pokok Sena area. Proceeding GEOSEA 98’, Ninth Regional Congress on Geology, Mineral and Energy Resource of Southeast Asia: 145-153.
[4] Zaiton Harun & Basir Jasin. 1999. Sempadan litostratigrafi batuan Paleozoik zon baratlaut Semenanjung Malaysia. Dynamic Stratigraphy & Tectonics Of Peninsular Malaysia- Seminar II, The Western Belt & Paleozoic of Peninsular Malaysia: 101-104
[5] Abdul Hadi, A. R. 1999. The Lower Permian ‘Passage Beds’ of the Kubang Pasu Formation,Perlis: Facies, stratification and significance. Dynamic Stratigraphy and Tectonic of Peninsular Malaysia- Seminar II: The Western Belt and Paleozoic of Peninsular Malaysia: 87-100.
[6] Abdul Hadi, A. R. 1999. The upper paleozoic Singa-Kubang Pasu mega-sequence: some thoughts on basin initiation, depositional and tectonic hostory. Dynamic Stratigraphy and Tectonic of Peninsular Malaysia- Seminar II: The Western Belt and Paleozoic of Peninsular Malaysia: 58-68
[7] Basir Jasin, Zaiton Harun & Siti Norhajar Hasan. 2003. Black siliceous deposits in Peninsular Malaysia: their occurance and significance. Annual Geological Conference 2003 46: 149-154
[8] Foo, K. Y. 1983. The Paleozoic rocks of Peninsular Malaysia-Stratigraphy and correlation. Proceeding of the Workshopon Stratigraphy Correlation of Thailand and Malaysia 1: 1-19.
[9] Hassan, M. H. & Lee, C. P. 2002. Stratigraphy of the Jentik Formation, the transitional sequence from the Setul Limestone to the Kubang Pasu Formation at Guar Sanai, Kampung Guar Jentik, Beseri, Perlis – a preliminary study. Geological Society of Malaysia Annual Geological Conference 2002: 169-178.
[10]Kobayashi, T. & Hamada, T. 1973. Cyrtosymbolids (Trilobita) from the Langgon Red Beds in Northwest Malaya, Malaysia. Geology & Palaeontology of Southeast Asia 12: 1-28.
Published
2016-12-01
How to Cite
SURYADI, Adi. Fault analysis to Determine Deformation History of Kubang Pasu Formation at South of UniMAP Stadium Hill, Ulu Pauh, Perlis, Malaysia. Journal of Geoscience, Engineering, Environment, and Technology, [S.l.], v. 1, n. 1, p. 1-6, dec. 2016. ISSN 2541-5794. Available at: <http://journal.uir.ac.id/index.php/JGEET/article/view/1>. Date accessed: 22 sep. 2019. doi: https://doi.org/10.24273/jgeet.2016.11.1.