000			01184nam a2200205 4500
001			0000002816
008			111108 1973 eng d
040			_aJMGHQ
090	0	0	_a553.6109595123 _bFAT
100	0		_aFateh Chand
245	1	0	_aFollow-up investigation of clays in Pahang Tenggara, Bukit Ibam _cFateh Chand, Ong Wee Seck.
260			_c1973
300			_a3p. _bill. _c33cm
520			_aField investigations have revealed that these clays which are residual in origin, are widespread in gently undulating areas underlain by argillaceous and fine-grained tuffaceous rocks. The thickness of the clays are variable, from 8 feet to some 52 feet, depending on the lithology of the underlying rocks and the topography. The laterite horizon encountered in most holes varies from 0 to 10 feet thick, thus reducing the thickness of usable clays. It is, perhaps pertinent to point out that in some areas narrows silty and sandy bands occur within the clay horizon.
650		0	_aSediments (Geology) _zPahang _zBukit Ibam
650		0	_aMineral industries _zPahang _zBukit Ibam
650		0	_aClay _zPahang _zBukit Ibam
651		0	_aBukit Ibam (Pahang)
700	1		_aOng, Wee Seck
999			_c22741 _d22741