000			01708nam a22001697a 4500
008			160218t2016 my 000 0 may
020			_a978-983-44396-9-9
100			_bZainol bin Husin and Mohammed Hatta bin Abd. Karim
245			_aGeologi dan sumber mineral kawasan Kuala Nerang, Kedah Darul Aman
250			_aLaporan peta 17
260			_aKuala Lumpur: _b Jabatan Mineral dan Geosains Malaysia, _c2010
300			_aill. 112 p. 30.3 cm x 21.5 cm.- _eAccompanying material: Geological map (Kuala Nerang .- New Series L 7010.- Sheet 1, Scale 1:63,360, 2010)
500			_bAbstract. The Kuala Nerang area situated at the north eastern part of the State of Kedah is covered by the New Series Topographic Sheet 1. The total area covered by the map sheet is about 1,215 km of which 980 km belonging to Malaysia was mapped. The rest of the map sheet area belonging to Changwatt Songkhla of Thailand was not mapped. Two sedimentary rock units were recognised in the mapped area namely, Kubang Pasu Formation and Semanggol Formation. The Kubang Pasu Formation of Carboniferous age is the oldest rock unit in the area. The formation dominates the western part of the area. The unit is predominantly made up of arenaceous and argillaceous rocks with minor amounts of siliceous rocks. The age of this formation was correlated to the rocks of the Kubang Pasu Formation that are well-exposed in the Map Sheet 152, Jitra, which is to the west of the study area. Overlying the Kubang Pasu Formation is the Semanggol Formation which is a flysch type deposit. It consists
648			_xGeology _yKedah _zKuala Nerang
650			_xMines and mineral resources _yKedah _zKuala Nerang
942			_2ddc _k555.9 ZAI
999			_c2 _d2