Rompin Mining Co. Ltd. geological report on the area between Bukit Pesagi & Bukit Sanlong B. Summers.
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TextPublisher: 1964Description: 12p. ill. 33cmSubject(s): Mineral industries -- Pahang | Iron ore -- Geology -- Pahang | Bukit Pesagi (Pahang) | Bukit Sanlong (Pahang)Summary: Seven deposits of iron ore are known in the area. They have been prospected by pitting, tunneling and diamond drilling. In addition airborne and ground magnetometric surveys have been carried out. Two of the deposits are of vein type and consists of specularite and pyrite, enriched by oxidation at and near outcrop. The others are of lateritic formation but are in most cases believed to be related to pyritic veins. It is considered that all the ore is genetically related to intrusions of diorite, which is often magnetiferous. Forty eight diamond drill holes were put down, totalling 7589 feet.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 553.0959512341 SUM (Browse shelf) | Available | 00003779 |
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| 553.0959512322 KAJ Kajian susulan prospek Batu Yon Kuala Lipis Pahang | 553.0959512323 TEO Bahagian mineralogi dan petrologi thoriarite from Bukit Keluang area, Raub, Pahang | 553.0959512341 MSI Geology dan sumber - sumber mineral sebahagian syit 108, Kuala Rompin dan sebahagian syit 117, Sungai Selai | 553.0959512341 SUM Rompin Mining Co. Ltd. geological report on the area between Bukit Pesagi & Bukit Sanlong | 553.0959521 INS Upgrading of iron - ore tailings | 553.0959521 REPsab 1987 Report on the mineral exploration in Sabah, Malaysia (phase II). | 553.0959521 REPsab 1988 Report on the mineral exploration in Sabah, Malaysia |
January, 1964.
Seven deposits of iron ore are known in the area. They have been prospected by pitting, tunneling and diamond drilling. In addition airborne and ground magnetometric surveys have been carried out. Two of the deposits are of vein type and consists of specularite and pyrite, enriched by oxidation at and near outcrop. The others are of lateritic formation but are in most cases believed to be related to pyritic veins. It is considered that all the ore is genetically related to intrusions of diorite, which is often magnetiferous. Forty eight diamond drill holes were put down, totalling 7589 feet.
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