000 | 01089nam a2200193 4500 | ||
---|---|---|---|
001 | 0000002873 | ||
008 | 111202 1993 eng d | ||
040 | _aJMGHQ | ||
090 | 0 | 0 |
_a555.9522 _bSUH |
100 | 0 | _aSuhaimi Yusoff | |
245 | 1 | 0 |
_aProgress report _bregional geological mapping of the Sungai Katibas area, Sarawak _cSuhaimi Yusoff |
260 | _c1993 | ||
300 |
_a7p. _bmaps,photos(col.) _c30cm |
||
504 | _aIncludes bibliographical references | ||
520 | _aSungai Katibas in underlinedby the kapit Members of Belaga Formation. The Kapit member is composed of argillite,shale,phyllite and greywacke,deposited during Paleocene Lower E ocene time (Le ichti et al,1960).The bedding are highly deformed with folding and faulting.Overall, strike of the bedding is WSW-ENE direction with NWW-SSE dipping direction. The lineament analysis shows that the compression force acting on the bedding is in the direction of 170c and 350c | ||
650 | 0 |
_aGeological mapping _zSarawak _zKatibas,Sungai |
|
650 | 0 |
_aRiver sediments _zSarawak _zKatibas,Sungai |
|
651 | 0 | _aKatibas,Sungai(Sarawak) | |
999 |
_c23201 _d23201 |