Status of uranium exploration in Peninsular Malaysia Fateh Chand
Material type: TextPublisher: 1981Description: 15 p. 30 cmSubject(s): Minerals -- Malaysia | Uranium -- Malaysia -- GeologySummary: The date some 20,000 km2 have been sampled in Kelantan, Pahang and Terengganu on a reconnaissance scale and about 20000 samples have been collected. An initial appraisal of part of the data collected has outlined several favourable areas in Pahang and Kelantan for further work. The findings show taht in aadition to the mesozorc sediments certain granitic bodies within the central Belt area have shown anomalous radioactivity not only from spectrometry, but also from stream sediment heavy mineral stream concentrate and water geochemistry,Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
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Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 553.4932095951 FAT (Browse shelf) | Available | 00003740 |
Browsing JMG IBUPEJABAT shelves, Shelving location: Open Shelf, Collection: Open Shelf Close shelf browser
553.493209595 TAY Uranium exploration and potential Peninsular Malaysia | 553.493209595 TAY Uranium exploration and potential Peninsular Malaysia | 553.493209595 TAY Uranium exploration and potential Peninsular Malaysia | 553.4932095951 FAT Status of uranium exploration in Peninsular Malaysia | 553.493209595114 ALL Alleged uranium ore at Fook Wan Foh mine at Chendering | 553.493209595114 ALL Alleged uranium ore at Fook Wan Foh mine at Chendering | 553.493209595114 KHO Prospect for uranium in the Klian Intan area, Upper Perak, Malaysia |
No. CB 02/1981
The date some 20,000 km2 have been sampled in Kelantan, Pahang and Terengganu on a reconnaissance scale and about 20000 samples have been collected. An initial appraisal of part of the data collected has outlined several favourable areas in Pahang and Kelantan for further work. The findings show taht in aadition to the mesozorc sediments certain granitic bodies within the central Belt area have shown anomalous radioactivity not only from spectrometry, but also from stream sediment heavy mineral stream concentrate and water geochemistry,
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