Progress report regional geological mapping of the Bukit Goram area, Sarawak Abdul Hadi Abdul Rahman
Material type:
TextPublisher: 1999Description: 16p. col., ill., map, photos (col.) 30cmSubject(s): Sediments (Geology) -- Sarawak -- Bukit Goram | Geology -- Sarawak -- Bukit Goram | Bukit Goram (Sarawak)Summary: The study area is underlain by the Kapit Member and the Layar Member of the Belaga Formation. The Layar Member is Late Cretaceous age (Liechti et al., 1960) and composed of slate, phyllite, shale and greywacke which covering about 25% of the studied area while the Kapit Member is composed of argillite, slate, phyllite, shale and greywacke which is deposited during Palae ocene-Early Eocene. Rocks units in this area are highly deformed where the beds was folded and faulted.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 555.95222 AHA (Browse shelf) | Available | 00003920 |
Browsing JMG IBUPEJABAT shelves, Shelving location: Open Shelf, Collection: Open Shelf Close shelf browser
| 555.952211 TAN The geology of Kuching Town, with some aspect of the engineering geology | 555.952212 RIC Reconnaissance investigation of geosite | 555.952213 LIN General geology of Batu Kawa/Tundong/Lundu road area | 555.95222 AHA Progress report | 555.95222 EDWbp Pemetaan geologi terain kawasan Binong Pass, Serian, bahagian Samarahan, Sarawak | 555.95222 EDWkt Pemetaan geologi terain kawasan Kakai Tarat, Serian, bahagian Samarahan, Sarawak | 555.95222 EDWse Pemetaan geologi terain kawasan Lanchang, Serian, bahagian Samarahan, Sarawak |
Includes bibliographical references
The study area is underlain by the Kapit Member and the Layar Member of the Belaga Formation. The Layar Member is Late Cretaceous age (Liechti et al., 1960) and composed of slate, phyllite, shale and greywacke which covering about 25% of the studied area while the Kapit Member is composed of argillite, slate, phyllite, shale and greywacke which is deposited during Palae ocene-Early Eocene. Rocks units in this area are highly deformed where the beds was folded and faulted.
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