000 02210nam a22001937a 4500
008 160218t2012 my 000 0 may|
020 _a978-967-0159-11-9
082 _a555.9 JAS
100 _bJasmi bin Ab. Talib
245 _aGeologi dan sumber mineral kawasan Kuala Tembeling, Pahang Darul Makmur
250 _aLaporan peta 23
260 _aKuala Lumpur:
_bJabatan Mineral dan Geosains Malaysia, Kementerian Sumber Asli dan Alam Sekitar,
_c2012.
300 _ai - xi.- 108 p.- ill.- 30.3 cm .-Hard cover.-
_eAccompanying material: Geological Map (Kuala Tembeling.- New Series L 7010.- Sheet 69.- Scale 1 : 63,360)
500 _aPrice: RM 100.00
942 _2ddc
520 _aAbstract. The study area is located at central Pahang covering the whole topographic map Sheet 69 Kuala Tembeling, Series L 7010 with an area of coverage approximately 1,200 km. It is dominated by low to medium terrain with 60% of the area covered by primary and secondary forest. Six lithostratigraphic units and intrusive rocks had been identified in the study area. The lithostratigraphic units are the Telong Formation., Semantan Formation, Kaling Formation, Kerum Formation, Mangking Sandstone and Termus Shale. In the study area, the Telong Formation is divisible into two informal members namely the Kayu Ara member and Kenong member. The Kayu Ara member is essentially made up of argillaceous and pyroclastic rocks, whereas the Kenong member consists mainly of calcareous rocks. The Telong Formation was probably deposited during late Middle Permain to Middle Triassic. The age is based on the occurrences of algae, foraminiferas and corals found in the Kenong member. More than half of this area is covered by the Semantan and Kaling Formations. The Semantan Formation comprises interbedded argillaceous and tuffs whilst the Kaling Formation is composed predominantly of argillaceous, arenaceous and rudaceous rocks. The presence of Posidonia, Daonella, Myophoris and ammonites indicates the age of the Semantan Formation is early Middle Triassic to Late Triassic.
648 _xGeology
_yMalaysia
_zKuala Tembeling, Pahang
650 _xMineral Resources
_yMalaysia
_zKuala Tembeling, Pahang
999 _c868
_d868