Template for for the Jurnal Teknologi
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Perak Development Experience: the Way Forward
International Journal of Academic Research in Business and Social Sciences December 2013, Vol. 3, No. 12 ISSN: 2222-6990 The Perak Development Experience: The Way Forward Azham Md. Ali Department of Accounting and Finance, Faculty of Management and Economics Universiti Pendidikan Sultan Idris DOI: 10.6007/IJARBSS/v3-i12/437 URL: http://dx.doi.org/10.6007/IJARBSS/v3-i12/437 Speech for the Menteri Besar of Perak the Right Honourable Dato’ Seri DiRaja Dr Zambry bin Abd Kadir to be delivered on the occasion of Pangkor International Development Dialogue (PIDD) 2012 I9-21 November 2012 at Impiana Hotel, Ipoh Perak Darul Ridzuan Brothers and Sisters, Allow me to briefly mention to you some of the more important stuff that we have implemented in the last couple of years before we move on to others areas including the one on “The Way Forward” which I think that you are most interested to hear about. Under the so called Perak Amanjaya Development Plan, some of the things that we have tried to do are the same things that I believe many others here are concerned about: first, balanced development and economic distribution between the urban and rural areas by focusing on developing small towns; second, poverty eradication regardless of race or religion so that no one remains on the fringes of society or is left behind economically; and, third, youth empowerment. Under the first one, the state identifies viable small- and medium-size companies which can operate from small towns. These companies are to be working closely with the state government to boost the economy of the respective areas. -
Chapter 1 Introduction
CHAPTER 1 INTRODUCTION 1.0 INTRODUCTION 1.1 Background Study Tin mining is one of the oldest industries in Malaysia. As what had been researched by James R.Lee (2000), the tin mining started since 1820s in Malaysia after the arrival of Chinese immigrants. The Chinese immigrants settled in Perak and started tin mines. Their leader was the famous Chung Ah Qwee. Their arrival contributed to the needed labour and hence the growth of the tin mining industry. Tin was the major pillars of the Malaysian economy. Tin occurs chiefly as alluvial deposits in the foothills of the Peninsular on the western site. The most important area is the Kinta Valley, which includes the towns of Ipoh, Gopeng, Kampar and Batu Gajah in the state of Perak. But that was long ago before price of tin had fallen greatly and high cost of mining had shutdown the industry. What is left now is the abandoned mine site scattered all over Perak. Some mines are far from populated area and some are in the population itself such as Universiti Teknologi PETRONAS (UTP). The campus is located on land that was once an active tin mining site. The residual of past activities can be seen where number of mining ponds can be found scattered in the vicinity of UTP. The main concern from geologist and nature agencies are the identification of Potentially Toxic Elements (PTEs) and the level of concentration for each element found in the area. Until now, there are only a few numbers of studies in Malaysia that has been done on data collection of PTEs and elevated content of PTEs in former mine. -
Higher-Resolution Biostratigraphy for the Kinta Limestone and an Implication for Continuous Sedimentation in the Paleo-Tethys, Western Belt of Peninsular Malaysia
Turkish Journal of Earth Sciences Turkish J Earth Sci (2017) 26: 377-394 http://journals.tubitak.gov.tr/earth/ © TÜBİTAK Research Article doi:10.3906/yer-1612-29 Higher-resolution biostratigraphy for the Kinta Limestone and an implication for continuous sedimentation in the Paleo-Tethys, Western Belt of Peninsular Malaysia 1,2, 2 3 4 2 5 Haylay TSEGAB *, Chow Weng SUM , Gatovsky A. YURIY , Aaron W. HUNTER , Jasmi AB TALIB , Solomon KASSA 1 South-East Asia Carbonate Research Laboratory (SEACaRL), Department of Geosciences, Faculty of Geosciences and Petroleum Engineering, Universiti Teknologi PETRONAS, Bandar Seri Iskandar, Perak Darul Ridzuan, Malaysia 2 Department of Geosciences, Faculty of Geosciences and Petroleum Engineering, Universiti Teknologi PETRONAS, Bandar Seri Iskandar, Perak Darul Ridzuan, Malaysia 3 Lomonosov Moscow State University, Moscow, Russian Federation 4 Department of Applied Geology, Western Australian School of Mines, Curtin University, Perth, Australia 5 Department of Applied Geology, School of Applied Natural Sciences, Adama Sciences and Technology University, Adama, Ethiopia Received: 29.12.2016 Accepted/Published Online: 21.09.2017 Final Version: 13.11.2017 Abstract: The paleogeography of the juxtaposed Southeast Asian terranes, derived from the northeastern margins of Gondwana during the Carboniferous to Triassic, resulted in complex basin evolution with massive carbonate deposition on the margins of the Paleo- Tethys. Due to the inherited structural and tectonothermal complexities, discovery of diagnostic microfossils from these carbonates has been problematic. This is particularly the case for the Kinta Limestone, a massive Paleozoic carbonate succession that covers most of the Kinta Valley in the central part of the Western Belt of Peninsular Malaysia. -
Cenozoic Stratigraphy, Sedimentation and Tectonic Setting, Onshore Peninsular Malaysia: a Review Sani Ado Kasim1,2,* Mohd Suhaili Ismail1 Ahmad Mohamed Salim1
Advances in Engineering Research, volume 200 Proceedings of the Third International Conference on Separation Technology 2020 (ICoST 2020) Cenozoic Stratigraphy, Sedimentation and Tectonic Setting, Onshore Peninsular Malaysia: A Review Sani Ado Kasim1,2,* Mohd Suhaili Ismail1 Ahmad Mohamed Salim1 1Department of Geoscience, Universiti Teknologi PETRONAS, 32610 Bandar Seri Iskandar, Malaysia 2Department of Geology, Bayero University Kano, PMB 301, Kano, Nigeria *Corresponding author. Email:[email protected] ABSTRACT Cenozoic sediments in Peninsular Malaysia occur along the western and eastern part of the Peninsular as onshore basins and in the South China Sea and the Straits of Malacca as offshore basins. The study is about reviewing the stratigraphy, sedimentation and tectonic pattern of the onshore Cenozoic basins/sediments, Peninsular Malaysia. This is with the aim of updating and establishing missing information and proposing future research direction. The Cenozoic sediments occupy 20 percent of the landmass of Peninsular Malaysia, with Quaternary deposits dominating. The Tertiary rocks/basins, which are Eocene to Oligocene in age, occur as pull-apart basins in seven localities (Batu Arang, Bukit Arang, Kampung Durian Chondong, Enggor, Layang-Layang, Lawin and Kluang-Niyor). Siliciclastic sedimentary rocks (conglomerates, sandstones, siltstone and shales/mudstones) are the dominant rock types in the Tertiary stratigraphy. Coal seams especially the low-grade types have been reported in these Tertiary basins. The basins are half graben or isolated circular depression aligned to major fault zones. Quaternary sediments occupy east and west coastland with minor occurrences within river valleys onshore. They consist of unconsidered boulders, gravels, sand, silts and clays. The Quaternary formations (Simpang, Kempadang, Gula and Beruas) are distributed in and around North Kedah and Perlis, South Kedah and Penang, Perak, Kinta Valley, Selangor, Kuala Lumpur, Negeri Sembilan and Malacca, west, east and central Johor, Terengganu and Kelantan. -
2 Geology of Peninsular Malaysia
2 GEOLOGY OF PENINSULAR MALAYSIA 2.1 INTRODUCTION Peninsular Malaysia has traditionLlly been subdivided into NNW-SSE longitudinal belts on the basis of stratigraphy, mineralisation, geological structure, geological history and tectonic evolution . Scrivenor (19:;8) subdivided the Peninsula into three elongate belts on the basis of mineralisation: a western tin belt, a central gold belt and an eastern tin belt. Hutchison (1977) divided the Peni isula into four major tectonic subdivisions on the basis of different tectonic histories; the '1Vestern Stable Shelf, the Main Range Belt, the Central graben, and the Eastern Belt. Fo ) (1983) divided the Peninsula into four zones on the basis of differences in stratign phy. Khoo and Tan (1983) proposed a threefold subdivision; a Western Belt, Central Belt and an Eastern Belt on the basis of differences in stratigraphy and geological histoi y within Peninsular Malaysia. Within this threefold subdivision, Khoo and Tan (1983' further divided the Western Belt into two regions: a northwest sector and a Kinta-Ma acca sector. Tjia and Harun (1985) recognised four structural domains within the Peninsula. They defined Northwest, West, Central and Eastern structural domains. Within all the above subdivision schemes, the boundary between the eastern and central "belts" is taken as the Lebir Fault 2 one, and the boundary between the central and western "belts" is the Bentong-Raub line of Hutchison (1975). As previously stated (Chapter 1.5.2), Metcalfe (1988) proposed that Peninsular Malaysia consisted of two continental terra les, a western Gondwanan affinity continental terrane (Sibumasu) and an eastern Cathaysian affinity continental terrane (Indochina/East Malaya) Chapter 2: Geology of Peninsular Malaysia (Fig. -
Kinta Valley, Perak, Malaysia
Geological Society of Malaysia c/o Department of Geology University of Malaya, 50603 Kuala Lumpur +603-79577036 (voice) +603-79563900 (fax) [email protected] http://www.gsm.org.my/ PERSATUAN GEOLOGI MALAYSIA GEOLOGICAL SOCIETY OF MALAYSIA COUNCIL 2013-2014 PRESIDENT : PROF. DR. JOY JACQUELINE PEREIRA (UKM) VICE-PRESIDENT : DR. MAZLAN MADON (PETRONAS) IMM. PAST PRESIDENT : DATO’ YUNUS ABDUL RAZAK (JMG) SECRETARY : MR. LING NAN LEY (JMG) ASSISTANT SECRETARY : MR. LIM CHOUN SIAN (UKM) TREASURER : MR. AHMAD NIZAM HASAN (GEOSOLUTION RESOURCES) EDITOR : ASSOCIATE PROF. DR. NG THAM FATT (UM) COUNCILLORS : MR. TAN BOON KONG (CONSULTANT) DR. NUR ISKANDAR TAIB (UM) DR. TANOT UNJAH (UKM) DR. SAMSUDIN HJ TAIB (UM) DR. MEOR HAKIF AMIR HASSAN (UM) MR. ROBERT WONG (PETRONAS) MR. NICHOLAS JACOB (JKR) MR. ASKURY ABD KADIR (UTP)* NATIONAL GEOSCIENCE CONFERENCE 2013 ORGANIZING COMMITTEE CHAIRMAN : DR. KAMALUDIN B. HASSAN (JMG PERAK) TECHNICAL CHAIRMAN : MR. HJ. ASKURY B. ABD. KADIR (UTP) TREASURER : MR. AHMAD NIZAM B. HASAN (GSM) SECRETARY/MEDIA : MS SUZANNAH BT AKMAL (JMG PERAK) ASST. SECRETARY : MR. MOHD. SHAHRIZAL B. MOHAMED SHARIFODIN (JMG PERAK) REGISTRATION : MR. LING NAN LEY (GSM) MS ANNA LEE (GSM) PRE-CONFERENCE FIELDTRIP AND : MR. HAJI ISMAIL B. IMAN (JMG PERAK) SPOUSE PROGRAM SPONSORSHIPS : MR AHMAD ZUKNI B. AHMAD KHALIL (JMG MALAYSIA) TEXT FOR SPEECHES : TUAN RUSLI B. TUAN MOHAMED (JMG PERAK) HOTEL AND ACCOMODATION : MR. MOHAMAD SARI B. HASAN (JMG PERAK) PROTOCOL AND SOUVENIRS : MS. MARLINDA BT DAUD (JMG MALAYSIA) COMMITTEE MEMBERS : MR. YUSNIN B. ZAINAL ABIDIN (IPOH CITY COUNCIL) MR SAW LID HAW (PERAK QUARRIES ASSOC.) PPeerrssaattuuaann GGeeoollooggii MMaallaayyssiiaa GGeeoollooggiiccaall SSoocciieettyy ooff MMaallaayyssiiaa PPrroocceeeeddiinnggss ooff tthhee NNAATTIIOONNAALL GGEEOOSSCCIIEENNCCEE CCOONNFFEERREENNCCEE 22001133 Kinta Riverfront Hotel and Suites, Ipoh 8-9th June 2013 Edited by: Nur Iskandar Taib Co-organizers: Copyright: Geological Society of Malaysia, 2013-05-29 All rights reserved. -
The Spatial Configuration of Private Investments by Economic Actors in Perak
The spatial configuration of private investments by economic actors in Perak A consideration of centricity of the regional urban system of Southern Perak (Peninsular Malaysia) Luka Raaijmakers (6314554) Under supervision of dr Leo van Grunsven Faculty of Geosciences Department of Human Geography and Planning Master’s degree in Economic Geography Specialisation in Regional Development & Policy November 2019 Page | 2 Acknowledgements This thesis is part of the joint research project on regional urban dynamics in Southern Perak (Peninsular Malaysia). The project is a collaboration between Utrecht University (The Netherlands) and Think City Sdn Bhd (Malaysia), under supervision of dr Leo van Grunsven and Matt Benson. I would like to thank dr Leo van Grunsven for his advice related to scientific subjects and his efforts to make us feel at home in Malaysia. Also, I would like to thank Matt Benson and Joel Goh and the other colleagues of Think City for the assistance in conducting research in – for me – uncharted territory. I would like to address other words of thanks to the Malaysian Investment Development Authority, Institut Darul Ridzuan and all other political bodies that have proven to be valuable as well as economic actors for their honesty and openness with regard to doing business in Malaysia/Perak. Finally, the fun part of writing a master’s thesis in Malaysia, apart from obviously living abroad on a vibrant island, was the part of doing research. This required a little creativity, some resilience and even more perseverance. This could not have been done without the other student members of the research team that took part in the collective effort of unravelling the urban system of Perak by using the knowledge we have gained in our years as academics. -
The Importance and Significance of Heritage Conservation of the Ex-Tin Mining Landscape in Perak, Malaysia, the Abode of Grace
The Asian Conference on Asian Studies 2013 Official Conference Proceedings Osaka, Japan The Importance and Significance of Heritage Conservation of the ex-tin Mining Landscape in Perak, Malaysia, the Abode of Grace Suriati Ahmad, David Jones Deakin University, Australia 0134 The Asian Conference on Asian Studies 2013 Official Conference Proceedings 2013 Abstract The tin mining industry in Malaysia is one of its major exports and has been classified as its oldest industrial heritage. According to the Malaysian Department of Statistics, the mining sector continues to be significant, supplying basic raw materials to the construction and manufacturing sectors enabling Malaysia's economic growth. Until the late 1970s, Malaysia was the world's premier producer of tin, supplying some 40 per cent of the world's tin. Peninsular Malaysia contributes the highest percentage of tin mining production and the biggest mining area is situated in Perak, comprising Taiping of Larut district, Kinta Valley district (Ipoh, Gopeng, Kampar, Batu Gajah, Tronoh), Pahang and Selangor, which includes the capital of Malaysia, Kuala Lumpur. However, due to a global recession in 1929 to 1932 a severe decline occurred in this industry. This decline affected the price of tin that fell sharply due to a lack of demand from European markets and caused the closure of many tin mines. In 2011, the Malaysian Chambers of Mines indicated that in Peninsular Malaysia, there is more than 113,700 ha of ex-tin mining areas and the majority of these areas are former tin mining sites. With the current rapid development and modernization of Perak state, the insistence on the human needs has caused changes to its moribund tin mining landscapes. -
Review on Microfossil Records of the Kinta Valley Sequences Haylay Tsegab, Aaron W
Review on Microfossil Records of the Kinta Valley Sequences Haylay Tsegab, Aaron W. Hunter, Bernard J. Pierson, & Chow Weng Sum, Southeast Asia Carbonate Research Laboratory (SEACARL) Universiti Teknologi PETRONAS Abstract Kinta valley was a focus of interest in search of geological resources for the last ten decades. Most of those studies were oriented to reveal the genesis of tin mineralization. Few workers including the current authors have identified some micro faunal (bivalves, gastropods, rugose corals, foraminifera, crinoids) records for relative dating of the limestone sequences. Even though present day accessibility of the reported fossiliferous sites is limited; areas which are dated based on the fossil records in Chemor (Silurian to Devonian), near Batu Gajah (Devonian), Malim Nawar (Carboniferous), Tualang limestone (Carboniferous to Permian), Kampar (Permian), and Kampung Sungai Keruh (Permian), are part of the Kinta valley limestone. The age difference in the limestones is interpreted as a result of migration of the coral reefs in the palaeodepositional setting. This current study will review the fossil collections of the JMG in Ipoh in order to test these original age determinations. We will demonstrate how these historic collections and macrofossil will contribute to our new research project. Furthermore, we will outline how these data will contribute to our ongoing research into defining a reference stratigraphic section that will enable correlation between scattered outcrops in the western Belt of Peninsular Malaysia. Kinta valley was a focus of interest in search of geological resources for the last ten decades. Most of those studies were oriented to reveal the genesis of tin mineralization in the quaternary alluvium deposits and to optimize the industrial use of limestones. -
The Extreme Karstification of the Kinta Valley, West Malaysia
THE EXTREME KARSTIFICATION OF THE KINTA VALLEY, WEST MALAYSIA Ros Fatihah Muhammad Department of Geology, University Malaya, 50603 Kuala Lumpur, [email protected] Abstract Parts of lowland equatorial Southeast Asia are amongst Surface limestone makes up only about 7% of the whole the few areas of the world where possibly little or no karst area; the greater subsurface area lies beneath climatic change has taken place during the Quaternary thick alluvial sediments. The depth of the subsurface (Ashton, 1972; Gale, 1986; CLIMAP, 1976; Prell et varies from 9 m to more than 60 m, and shows various al., 1980). Paramananthan (1982) considers lateritic topographies from platforms with flat concordant soils formed during the Tertiary (Batchelor, 1979; Law tops to jagged sharp pinnacles with rounded tops. The and Leamy, 1966; Eyles, 1970 after Raj, 1982) to have ratio of surface to subsurface karst can be used as an developed during the Pleistocene through the deposition indication of the intensity of dissolution that occurs and of iron-coated materials that were derived by erosion of advanced degradation. Based on its association with from weathering profiles formed by intensive tropical tin-rich alluvium, it is believed that the karst in this area weathering. Some evidence for this Tertiary humid developed mostly under a pluvial environment and the tropical climate is seen in Mueller (1972), whose humid tropical conditions since the Tertiary. palynological analysis led to the conclusion that there was a uniformly humid climate throughout the Tertiary. Introduction The Kinta Valley in Perak, Peninsular Malaysia is However, it has been suggested that this study area important historically; the richest tin mine in the world was subject to repeated climatic variations and was located here. -
Brief Geological Field Guide to the Kinta Limestone, Kinta Valley, Perak
Brief geological field guide to the Kinta Limestone, Kinta Valley, Perak Malaysia Organized by: Southeast Asia Carbonate Research Laboratory, SEACARL The Department of Geosciences, Faculty Fundamental sciences, Information system Technology Universiti Teknologi PETRONAS November, 2019 Prepared by: Dr Haylay Tsegab Team members Dr Mirza Arshad Dr Haylay Tsegab Mr. Chee Meng Table of Contents I. Safety .................................................................................................................................................... 3 II. Time and venue (itinerary) ............................................................................................................. 4 III. Field excursion learning outcomes ................................................................................................ 4 IV. Introduction ..................................................................................................................................... 5 V. Geological and Stratigraphic Setting ................................................................................................ 5 VI. Post-depositional processes ............................................................................................................ 6 A. Dolomite distribution ............................................................................................................................ 7 B. Karsification ......................................................................................................................................... -
An Overview of Sinkhole Geohazard Incidence Recorded in the Kinta Valley Area, Perak
ASM Sc. J., 11, Special Issue 2, 2018 for SANREM, 19-28 An Overview of Sinkhole Geohazard Incidence Recorded in The Kinta Valley Area, Perak Ahmad Khairut Termizi1,2,3∗, Tuan Rusli Tuan Mohamed1 and Rodeano Roslee2,3 1Minerals and Geoscience Department of Malaysia (JMG-Malaysia), Jalan Penampang, 88999 Kota Kinabalu, Sabah, Malaysia 2Natural Disaster Research Centre (NDRC), University Malaysia Sabah (UMS), Jalan UMS, 88400 Kota Kinabalu, Sabah, Malaysia 3Faculty of Science and Natural Resources (FSSA), University Malaysia Sabah (UMS), Jalan UMS, 88400 Kota Kinabalu, Sabah, Malaysia This paper is prepared to provide an overview of the sinkholes geohazards that occurs quite often in the Kinta Valley area. By fact, the phenomenon of the sinkhole is a common in Kinta Valley as its compound in karsts environment with limestone bedrock underlain about 80% of the area. The occurrences of sinkholes always affected badly on urban development and caused economic loses to the owner or landlord. The record regarding the sinkholes in pass days was started informally through shorthand in the log book and personal diaries. Since the cases arose, Minerals and Geoscience Department of Malaysia (JMG-Malaysia) started proper documentation in year 1970s and until February 2012 there were 161 incidents and 288 sinkholes were recorded surrounding Kinta Valley. Preliminary interpretation shows that the development of sinkhole associated to the factors of subsurface geology, historic of site activities which related to mining, current land used status, also seasonal drastic change between dry and wet spell in local climate. Keywords: Sinkholes, Kinta Valley, Perak 1969). I. INTRODUCTION Smith (1999) defines the sinkhole as a hole The Kinta Valley has undergone an formation at a certain size from the top of the experience of sinkholes in very long time.