Progress report regional geological mapping of the Sungai Katibas area, Sarawak Suhaimi Yusoff
Material type: TextPublisher: 1993Description: 7p. maps,photos(col.) 30cmSubject(s): Geological mapping -- Sarawak -- Katibas,Sungai | River sediments -- Sarawak -- Katibas,Sungai | Katibas,Sungai(Sarawak)Summary: Sungai 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 350cItem type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
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Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 555.9522 SUH (Browse shelf) | Available | 00003932 |
Includes bibliographical references
Sungai 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
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