000			01500nam a2200229 4500
001			0000001465
008			110824s2010 eng d
040			_aJMGHQ
090	0	0	_a555.951232 _bMHI
100	0		_aMohamad Hafizzul Ishak
245	1	0	_aGeneral geology of Pos Belau, Jalan Cameron Highlands - Gua Musang _cBy Mohamad Hafizzul Ishak
260			_c2010
300			_axiv, 45 p. _bcol. ill., maps _c30 cm
504			_aIncludes bibliographical references
520			_aBased on this analysis, there are two facies of limestone at study area which is pelmicrite facies and biomicrite facies. Both classification of these facies are determined by using carbonate rock classification by Folk (1959, 1962). Microscopic analysis of sandstone also had determined that this sandstone is some kind of calcareous US sandstone, which is the usual sandstone but cemented with calcite. The study of macroscopic and microscopic of conglomerate determined that the clasts of the conglomerate are rounded to subrounded in shape and composed of calcareous clast. These analysis may help to interpret the diagenesis to determine the source of sandstone and conglomerate. It also may help in determining the environmental depositional of these rock.
650		0	_aPetrography _zKelantan _zPos Balau
650		0	_aRocks _xClassification
650		0	_aDissertations, Academic _zMalaysia
650		0	_aGeology _xresearch _zKelantan _zPos Balau
651		0	_aPos Belau (Kelantan)
651		0	_aGua Musang (Kelantan)
999			_c22191 _d22191