geology of peninsular malaysia

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Malaysia is a country which consists of two parts peninsular Malaysia and East Malaysia Sabah Sarawak or Borneo.

. Based on the stratigraphic record and characteristics the area of Peninsular Malaysia is d1 vided into four stratigraphic zones viz. Geological Evolution of Peninsular Malaysia TT. The usage of these terms is limited in recent works.

Department of Geology University of Malaya Kuala Lumpur Malaysia. Tectonically Peninsular Malaysia forms part of the Sunda Shield. The capital of Malaysia is Kuala Lumpur and divided into 12 states each having own capital town.

Its Triassic fold-mountain belt the spine of the Peninsula continues from eastern Burma through Thailand Peninsular Malaysia the Banka and Billiton Islands and eastwards into Indonesian Borneo. TAN Department of Geology University of Malaya Kuala Lumpur. Peninsular Malaysia can be divided into 3 longitudinal belts3 Western3 Central and Eastern3 each of which has its own distinctive characteristics and geological development.

Simplified regional geological map of Peninsular Malaysia. A total of about 32000 magnetic intensity data were obtained from Earth Magnetic Anomaly Grid EMAG2 covering an area of East Sumatra to part of South. Outline Geology of Peninsular Malaysia.

Inclusive of Geological Map of Peninsular Malaysia scale 1 000 000. Peninsular Malaysia is more accustomed to only light tremors. Granite emplacement and tectonic subdivision of Peninsular Malaysia CHARLES S.

Geology of Peninsular Malaysia 2009 Edited by CS. Lithostratigraphic units are described according to their distribution in each zone Figure 2 and Table 1. Malaysia is largely seismically stable with little modern history of volcanic activity being situated entirely on the Sunda tectonic plate between two major boundaries of the Australian Plate and Eurasian Plate in the west of Peninsular Malaysia and the Philippine Sea Plate and Eurasian Plate at Bornean Malaysia.

Kaling Formation was proposed by Ahmad J. Based on the Geological Map of Peninsular Malaysia Fig 2 the lithology are limestone shale sandstone and siltstone. I northwestern zone 11 western zone iii central zone atd iv eastern zone Figure l.

Magnetic data were processed to interpret the geology of Peninsular Malaysia especially in delineating the igneous bodies and structural lineament trends by potential field geophysical method. All the systems ranging from the Cambrian to the Quaternary are represented in. The map shows the limits of the tectono-stratigraphical Western Central and.

It is the first proposed for development on the basis of only one exploration well. The Central Belt region of Peninsular Malaysia covering mainly central Pahang and Johor is dominated by middle-upper Triassic flysch-like rocks which are thought to represent a fore-arc. Peninsular Malaysia can be subdivided into four major tectonic regions-the Western Stable Shelf the Main Range Belt the Central Graben and the Eastern Belt.

The climate is tropical characterised by uniformly high tempaerature and seasonal rainfall. Currently it produces from four different sandstone units namely the J-16 J-17 J-1820 and K-2030. Throughout Peninsular Malaysia in particular the Gemas Formation Jurong and Jelai Formation and Semantan Formation Kerdau Formation.

The Tinggi field is the fifth field put on production by Esso Production Malaysia Inc EPMI off the East Coast of Peninsula Malaysia.

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