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Geology and mineral resources of the Sungai Tekai Area, Pahang Darul Makmur (Record no. 1)

000 -LEADER
fixed length control field 02813nam a22001817a 4500
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 160218t2009 my 000 0 eng
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 978-983-44396-1-3
Terms of availability BPT
082 ## - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 555.9 KHO
100 ## - MAIN ENTRY--PERSONAL NAME
Numeration Khoo Han Peng
245 ## - TITLE STATEMENT
Title Geology and mineral resources of the Sungai Tekai Area, Pahang Darul Makmur
250 ## - EDITION STATEMENT
Edition statement Map Report 18
260 ## - PUBLICATION, DISTRIBUTION, ETC.
Place of publication, distribution, etc. Kuala Lumpur,
Name of publisher, distributor, etc. Minerals and Geoscience Department Malaysia, Ministry of Natural Resources and Environment,
Date of publication, distribution, etc. 2009
300 ## - PHYSICAL DESCRIPTION
Extent ill. 106 p.- 29.6 cm.-
Accompanying material Accompanying material: Geological map (Sungai Tekai.- New Series L 7010 Sheet 70 Scale 1 : 63,360)
500 ## - GENERAL NOTE
General note Price: RM 60.00<br/><br/>Abstract.<br/><br/>The Sg. Tekai area is underlain predominantly by a group of continental sediments. Only Bangak metasediments and Lempah Granite occur to the northeast. These continental sediments previously included in the Tembeling formation by B.N. Koopmans in 1968, are now shown to be mappable as four lithostratigraphic units named as the Kerum Formation, Lanis Conglomerate, Mangking Sandstone and Termus Shale. These constitute the Tembeling Group. The order of succession of these new units is worked out largely from defined. These sections, however, do not show the finer details due to the scarcity of outsrops or their continuity in this type of terrain and climate.<br/><br/>Plants fossils Gleichenoides gagauensis Kon'no and bivalves Trigonoides, T. Kodairai Kobayashi & Suzuki, and Trigonoides kodairai paucisulcatus Suzuki belonging to the Unionacea a Jurassic-Late Cretaceous age. These discoveriesshed new light on the age range (i.e. the upper limit) of the sediments which were previously commonly accepted to be no younger than Jurassic.<br/><br/>Field structural data confirm much of the major structures interpreted from the aerial photographs and Landsat imagery. Following Koopman's idea in 1968, structures have been widely used as the criteria in differentiating Gagau group sediments from 'Tembeling' type rocks for many years. This role of structures is cautioned and its significance explained in the light of new ideas on the structural aspect. An illustration is presented by the Sg. Pelandok area where a patch of very gently dipping rocks, geomorphologically resembling Gagau type sediments, are found to be, in fact of the Mangking Sandstone positioned at the trough of the Pelandok Syncline. The near horizontal or very gentle dip of the beds is due to this position within the fold and not necessarily an indication of another group of rocks.<br/><br/>Fresh water invertebrate fossils, the abundance of red beds throughout the sequence and sedimentary structures are all suggestive of a continental palaeoenvironment.<br/><br/>
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme
Classification part 555.9 KHO
648 ## - SUBJECT ADDED ENTRY--CHRONOLOGICAL TERM
General subdivision Geology
Chronological subdivision Pahang
Geographic subdivision Sungai Tekai
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
General subdivision Mineral Resources
Chronological subdivision Pahang
Geographic subdivision Sungai Tekai
Holdings
Withdrawn status Lost status Source of classification or shelving scheme Damaged status Not for loan Permanent Location Current Location Date acquired Cost, normal purchase price Total Checkouts Full call number Date last seen Price effective from Koha item type Public note
Available         BPT BPT 18/02/2016 100.00   555.9 KHO 18/02/2016 11/05/2019 Books Geological and mineral resources.