Geologi dan sumber mineral kawasan Yong Peng, Johor Darul Takzim (Record no. 851)
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000 -LEADER | |
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fixed length control field | 01924nam a22001817a 4500 |
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
fixed length control field | 161102t2015 my 000 0 may |
020 ## - INTERNATIONAL STANDARD BOOK NUMBER | |
International Standard Book Number | 978-967-0159-27-0 |
082 ## - DEWEY DECIMAL CLASSIFICATION NUMBER | |
Classification number | 555.9511922 WAH |
100 ## - MAIN ENTRY--PERSONAL NAME | |
Numeration | Wahid Abdul Rahman |
245 ## - TITLE STATEMENT | |
Title | Geologi dan sumber mineral kawasan Yong Peng, Johor Darul Takzim |
250 ## - EDITION STATEMENT | |
Edition statement | Laporan Peta 26 |
260 ## - PUBLICATION, DISTRIBUTION, ETC. | |
Place of publication, distribution, etc. | Kuala Lumpur: |
Name of publisher, distributor, etc. | Jabatan Mineral Dan Geoains Malaysia, |
Date of publication, distribution, etc. | 2015. |
300 ## - PHYSICAL DESCRIPTION | |
Extent | ill. 114 p.- 29.8 cm.- |
Accompanying material | Accompanying material: Geological map (Geological map of Yong Peng Area.- New Series L 7010. Sheet 123.- Scale 1: 63,360., 2015) |
500 ## - GENERAL NOTE | |
Executive Summary | Summary of Geology.<br/><br/>The Yong Peng area is bounded by latitude 1 49'N to 11'N, and longitude 102 59'E to 103 15'E, covering an area of approximately 1,230 km. The study area is located in the low-lying western-central part of Johor. <br/><br/>The Upper Permain Dohol formation that was deposited in a marine environment is the oldest rock unit in the study area. The formation consist mainly of shale, siltstone, pyroclastic rocks, and minor limestone which had undergone low grade metamorphism. The rocks are folded due to compression from more than one orogeny phase, and are well exposed in the eastern part of the study area. <br/><br/>Deposition of the Semantan Formation took place during the Middle to Late Triassic. The formation that occupies most of the southeastern, central and northern parts of the study area comprises shale. siltstone, mudstone, tuff, and some sandstone. Semantan Formation is underlain unconformably by the Dohol formation.<br/><br/>Igneous instrusion in the Yong Peng area took place during the Late Triassic, i.e. after the deposition of the Semantan Formation was completed. There are two groups of instrusive rocks, namely the Soga Granite and the Bekok Granite occupies the northeastern part.<br/><br/> <br/> |
942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
Source of classification or shelving scheme | |
648 ## - SUBJECT ADDED ENTRY--CHRONOLOGICAL TERM | |
General subdivision | Geology |
Chronological subdivision | Johor |
Geographic subdivision | Yong peng |
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
General subdivision | Mine and mineral resources |
Chronological subdivision | Johor |
Geographic subdivision | Yong Peng |
Withdrawn status | Lost status | Source of classification or shelving scheme | Damaged status | Not for loan | Permanent Location | Current Location | Shelving location | Date acquired | Coded location qualifier | Cost, normal purchase price | Total Checkouts | Full call number | Date last seen | Price effective from | Koha item type | Collection code | Copy number | Cost, replacement price |
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Available | BPT | BPT | General Stacks | 02/11/2016 | Rak A | 100.00 | 555.951 | 02/11/2016 | 02/11/2016 | Maps | ||||||||
Available | Staff Collection | JMG SABAH | JMG SABAH | Map Report and Memo | 24/09/2024 | 100.00 | 24/09/2024 | 24/09/2024 | Reference | Map Report and Memo | 1 | 100.00 |