Follow-up investigation of clays in Pahang Tenggara, Bukit Ibam Fateh Chand, Ong Wee Seck.
Material type:
TextPublisher: 1973Description: 3p. ill. 33cmSubject(s): Sediments (Geology) -- Pahang -- Bukit Ibam | Mineral industries -- Pahang -- Bukit Ibam | Clay -- Pahang -- Bukit Ibam | Bukit Ibam (Pahang)Summary: Field 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.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 553.6109595123 FAT (Browse shelf) | Available | 00003402 |
Total holds: 0
Browsing JMG IBUPEJABAT shelves, Shelving location: Open Shelf, Collection: Open Shelf Close shelf browser
| 553.6109595123 FAT Follow-up investigation of clays in the Sungai Kumai area, Pahang Tenggara | 553.6109595123 FAT Detailed investigation of clays in the Keratong area Pahang Tenggara | 553.6109595123 FAT Investigation of clays in Pahang Tenggara area | 553.6109595123 FAT Follow-up investigation of clays in Pahang Tenggara, Bukit Ibam | 553.6109595123 MSI Nota mengenai lempung di kawasan Felda Selendang, Pahang | 553.6109595123 ROH Kaolin, ball clay and common clay investigation in Pahang | 553.6109595123 YUS Kajian tinjauan lempung bebola di negeri Pahang |
Field 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.
There are no comments on this title.