000			01425nam a2200229 4500
001			0000001503
008			110914s2009 ab eng d
040			_aJMGHQ
090	0	0	_a551.095951122 _bSFA
100	0		_aSheikh Fadzil Mohamad
245	1	0	_aStructure, stratigraphy, and sedimentology of Mong Gajah area, along km 36.1 to km 41.6, Trans Eastern Kedah Interland Highway, Kedah _cSheikh Fadzil Mohamed
260			_c2009
300			_ax, 55 p. _bcol. ill., maps _c30 cm.
500			_aStudent project paper, May 2009
504			_aIncludes bibliographical references
520			_aThe area study consists of Semanggol formation which range in age from Lower Permian to Upper Triassic. The main lithology of the Semanggol formation that can be found in the study area is consist of interbedded sandstone - shale and conglomerate belonging to the rhytmite and conglomerate member respectively. The rhythmite member also known as turbidite sequence, can be further be divided into two main facies namely thick sandstone - thick shale which and thin sandstone - thin shale. The conglomerate member that is found in the study area can be clasified as poorly sorted, matric supported conglomerate.
610	2	0	_aProjek Lebuhraya Lingkaran Timur Kedah
650		0	_aSedimentation and deposition _zKedah
650		0	_aSediments (Geology) _zKedah
650		0	_aGeology _zKedah _xSurvey
650		0	_aGeology, Stratigraphic
999			_c22275 _d22275