Geologi dan sumber mineral kawasan Nanga Mujong, Sarawak: Menjelaskan lembaran peta 6314 : RAK (E11 / E12) (Record no. 849)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02140nam a22001577a 4500 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
| fixed length control field | 161027t2010 my 000 0 may |
| 100 ## - MAIN ENTRY--PERSONAL NAME | |
| Numeration | S. Thomson Galin |
| 245 ## - TITLE STATEMENT | |
| Title | Geologi dan sumber mineral kawasan Nanga Mujong, Sarawak: Menjelaskan lembaran peta 6314 : RAK (E11 / E12) |
| 250 ## - EDITION STATEMENT | |
| Edition statement | RMK 9. Projek Pementaan Geologi Negara.- JMG.SRW ( PGN ) 3/2010 |
| 260 ## - PUBLICATION, DISTRIBUTION, ETC. | |
| Place of publication, distribution, etc. | Kuala Lumpur: |
| Name of publisher, distributor, etc. | Jabatan Mineral dan Geosains Malaysia, Kementerian Sumber Asli dan Alam Sekitar, |
| Date of publication, distribution, etc. | 2010. |
| 300 ## - PHYSICAL DESCRIPTION | |
| Extent | ill. 154p.- 29.8 cm.- |
| Accompanying material | Included geological map (Sarawak Geological Map 1 : 50 000.- Nanga Mujong, 2010) |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Source of classification or shelving scheme | |
| 520 ## - SUMMARY, ETC. | |
| Summary, etc. | Abstract.<br/><br/>Geological mapping under the 9th Malaysia Plan was carried out in the Nanga Mujong Area, Kapit Division, Sarawak commenced in 2008. The main objective of the mapping was to explain in detail the geology of the area at a scale of 1 : 50 000. The information collected is useful for future development plans in the area.<br/><br/>A geological map was produced with this report. The first part of this report introduces briefly the geographical and social aspects of the area followed by the review of the previous and current geological work carried out in the sea. This report covers the information on rocks, stratigraphy, structural geology of the mapping area.<br/><br/>The area is underlain by the Layar Member, Kapit Member and Pelagus Member of the Cretaceous-Middle Eocene Belaga Formation. It consists of phyllite, slate, argillites, siltstone and sandstone. However in places are pockets of superficial deposits. The rocks in the area underwent low-grade regional metamorphism with decreasing degree of metamorphism northwards. It had been deformed producing folds, faults and joints caused by palaeostress that is approximately oriented north-northwest and south-southeast. Uplift caused the rock to be above sea-level and subjected to weathering and erosion that produces riverine deposit.<br/><br/>From the economic aspect, the Nanga Mujong area has sandstone and gravel deposits that may be utilised in future. |
| 648 ## - SUBJECT ADDED ENTRY--CHRONOLOGICAL TERM | |
| General subdivision | Geology |
| Chronological subdivision | Sarawak |
| Geographic subdivision | Nanga Mujong |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| General subdivision | Mineral resources |
| Chronological subdivision | Sarawak |
| Geographic subdivision | Nanga Mujong |
| Withdrawn status | Lost status | Source of classification or shelving scheme | Damaged status | Not for loan | Permanent Location | Current Location | Shelving location | Date acquired | Cost, normal purchase price | Total Checkouts | Date last seen | Price effective from | Koha item type |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Available | BPT | BPT | General Stacks | 27/10/2016 | 50.00 | 27/10/2016 | 27/10/2016 | Books |