000			01924nam a22001817a 4500
008			161102t2015 my 000 0 may
020			_a978-967-0159-27-0
082			_a555.9511922 WAH
100			_bWahid Abdul Rahman
245			_aGeologi dan sumber mineral kawasan Yong Peng, Johor Darul Takzim
250			_aLaporan Peta 26
260			_aKuala Lumpur: _bJabatan Mineral Dan Geoains Malaysia, _c2015.
300			_aill. 114 p.- 29.8 cm.- _eAccompanying material: Geological map (Geological map of Yong Peng Area.- New Series L 7010. Sheet 123.- Scale 1: 63,360., 2015)
500			_bSummary of Geology. The Yong Peng area is bounded by latitude 1 49'N to 11'N, and longitude 102 59'E to 103 15'E, covering an area of approximately 1,230 km. The study area is located in the low-lying western-central part of Johor. The Upper Permain Dohol formation that was deposited in a marine environment is the oldest rock unit in the study area. The formation consist mainly of shale, siltstone, pyroclastic rocks, and minor limestone which had undergone low grade metamorphism. The rocks are folded due to compression from more than one orogeny phase, and are well exposed in the eastern part of the study area. Deposition of the Semantan Formation took place during the Middle to Late Triassic. The formation that occupies most of the southeastern, central and northern parts of the study area comprises shale. siltstone, mudstone, tuff, and some sandstone. Semantan Formation is underlain unconformably by the Dohol formation. Igneous instrusion in the Yong Peng area took place during the Late Triassic, i.e. after the deposition of the Semantan Formation was completed. There are two groups of instrusive rocks, namely the Soga Granite and the Bekok Granite occupies the northeastern part.
942			_2ddc
648			_xGeology _yJohor _zYong peng
650			_xMine and mineral resources _yJohor _zYong Peng
999			_c851 _d851