Projek pemetaan geologi negara. Kawasan Bukit Karah, Sarawak, Malaysia: Menjelaskan lembaran peta 6016. : RAK (E14)) (Record no. 850)

000 -LEADER
fixed length control field 02600nam a22001577a 4500
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 161027t2010 my 000 0 may
100 ## - MAIN ENTRY--PERSONAL NAME
Numeration Luqman bin Kaluni
245 ## - TITLE STATEMENT
Title Projek pemetaan geologi negara. Kawasan Bukit Karah, Sarawak, Malaysia: Menjelaskan lembaran peta 6016. : RAK (E14))
250 ## - EDITION STATEMENT
Edition statement RMK 9 (2006 - 2010). Projek Pemetaan Geologi Negara.-JMG.SWK.( PGN ) 2/2010
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. 104p., 29.8 cm.-
Accompanying material Included Geological Map (Peta geologi kawasan Bukit Karah, Sarawak, Malaysia.- Skala 1 : 50 000.- 2010)
500 ## - GENERAL NOTE
General note Price: RM 50.00
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme
520 ## - SUMMARY, ETC.
Summary, etc. Abstract.<br/><br/>Geological mapping in the Bukit Karah area was been implemented from the beginning April 2008 until September 2009. Studies include various geological aspecta and related methods of geological mapping. Based map was obtained from Department of Survey and Mapping Malaysia (JUPEM) serial T738, sheet 6016 with scale 1 : 50 000. Study area covers an area of 900 km.<br/><br/>Bukit Karah area is covered by Paleogene and Neogene sediments. The Paleogene sediment consisting of the pelagus and Metah Member from Belaga Formation whilw Neogene sediments is consisting of the Begrih Formation and Liang Formation.<br/><br/>The Pelagus Member is the oldest unit and underlying southern part's area of Bukit Karah. Marine sediments that deposited in this Mid Paleocene unit formed by an interbedded sequence of sandstone mainly greywacke with, shale alternation, sandstone alternation and siltstone. Metah Member deposited during Mid Eocene-Late Eocene is consisting of alternation of shale and sandstone.<br/><br/>Begrih Formation aged Early Pliocene-Mid Pliocene underline a small area at the north of Bukit Karah area deposited in a marine environment. The Liang Formation is the youngest precipitated around Middle Pleistocene-Pleocene. This formation is consisting of interbedded sandstone with shale, sandy clay, clay and sandstone with pebble and lignite. This unit is scattered randomly at the north of Bukit Karah area.<br/><br/>The Pelagus and Metah Member separated by interfingering boundary. The Belaga Formation is generally trending northwest to southeast with the bedding pitch around 60 - 90 degrees. The ridgesin this area is parallel to this bedding plane unit.<br/><br/>The trend of the ridges in Liang Formation is southwest to northeast. This formation less folded. The Liang and Begrih Formation is separated by unconformity boundary.
648 ## - SUBJECT ADDED ENTRY--CHRONOLOGICAL TERM
General subdivision Geological Map
Chronological subdivision Malaysia
Geographic subdivision Sarawak, Bukit Karah
Holdings
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
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