A Stone and Bronze Tool Cave in Sabah
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“Fractured Basement” Play in the Sabah Basin? – the Crocker and Kudat Formations As Hydrocarbon Reservoirs and Their Risk Factors Mazlan Madon1,*, Franz L
Bulletin of the Geological Society of Malaysia, Volume 69, May 2020, pp. 157 - 171 DOI: https://doi.org/10.7186/bgsm69202014 “Fractured basement” play in the Sabah Basin? – the Crocker and Kudat formations as hydrocarbon reservoirs and their risk factors Mazlan Madon1,*, Franz L. Kessler2, John Jong3, Mohd Khairil Azrafy Amin4 1 Advisor, Malaysian Continental Shelf Project, National Security Council, Malaysia 2 Goldbach Geoconsultants O&G and Lithium Exploration, Germany 3 A26-05, One Residences, 6 Jalan Satu, Chan Sow Lin, KL, Malaysia 4 Malaysia Petroleum Management, PETRONAS, Malaysia * Corresponding author email address: [email protected] Abstract: Exploration activities in the Sabah Basin, offshore western Sabah, had increased tremendously since the discovery of oil and gas fields in the deepwater area during the early 2000s. However, the discovery rates in the shelfal area have decreased over the years, indicating that the Inboard Belt of the Sabah Basin may be approaching exploration maturity. Thus, investigation of new play concepts is needed to spur new exploration activity on the Sabah shelf. The sedimentary formations below the Deep Regional Unconformity in the Sabah Basin are generally considered part of the economic basement which is seismically opaque in seismic sections. Stratigraphically, they are assigned to the offshore Sabah “Stages” I, II, and III which are believed to be the lateral equivalents of the pre-Middle Miocene clastic formations outcropping in western Sabah, such as the Crocker and Kudat formations and some surface hydrocarbon seeps have been reported from Klias and Kudat peninsulas. A number of wells in the inboard area have found hydrocarbons, indicating that these rocks are viable drilling targets if the charge and trapping mechanisms are properly understood. -
The Paleogene Basins of Sabah, East Malaysia
AAPG II/fertli/fumal Cu4ermc( d EYhibifum '94 AJ/g/l.lf21-24, 1994, KJ/ala Lumpur, Maltzy"iLl The Paleogene basins of Sabah, East Malaysia F. TONGKUL Earth Science Department Universiti Kebangsaan Malaysia, Sabah Campus Locked Bag No. 62, 88996 Kota Kinabalu, Sabah, Malaysia Abstract: The Paleogene basins of Sabah developed in two stages, represented by early and late Paleogene sediments, in association with NW-SE compressional deformation during the late Mesozoic and Middle Eocene. The earlier deformation produced a wide elongate basin trending NE-SW bordered by a continental block to the NW and an emergent oceanic basement to the SE. The basin became the depositional sites of shallow to deep water early Paleogene sediments. The later deformation divided the earlier basin into two parallel basins (Outer and Inner basins) also trending NE-SW. Both basins were independently filled by shallow to deep water late Paleogene sediments derived axially from the southwest and laterally from the northwest and southeast. These basins were finally closed during the early Miocene resulting in the Paleogene fold-thrust belt of Sabah. INTRODUCTION Sea oceanic crust in the SE (Fig. 1). The sediments covers most of western, northern and central Sabah The Paleogene basins of Sabah here refers to while in eastern Sabah the sediments are not clearly the depositional sites of thick Paleogene sediments mapped out due to the presence of extensive melange forming the mountainous belt of Sabah. Unlike deposits (Fig. 2). The Paleogene sediments continue most of the younger basins, the configuration of the southward onland into Sarawak and NE Paleogene basins were not preserved but greatly Kalimantan (Hamilton, 1979; Hutchison, 1989) and modified by compressional tectonics. -
Curriculum Vite
BIODATA Ejria Binti Saleh Senior Lecturer, Borneo Marine Research Institute, Universiti Malaysia Sabah, Malaysia BIO SUMMARY - LIM AI YIM - MALAYSIA CURRICULUM VITE PERSONAL INFORMATION Name Name of Current Employer: Borneo Marine Research Institute Ejria Binti Saleh Universiti Malaysia Sabah Corresponding Address: E-mail: Borneo Marine Research Institute, [email protected]/[email protected] Universiti Malaysia Sabah, 88999 Kota Kinabalu, Sabah Malaysia Tel: 6088-320000 ext: 2594 Fax: 6088-320261 NRIC: 710201-12-5042 Nationality: Malaysian Date of Birth: 01 January 1971 Sex: Female ACADEMIC QUALIFICATION Diploma/Degree Name of University Year Major Doctor of Philosophy Universiti Malaysia 2007 Physical Oceanography Sabah, Malaysia. Master Science University of Liverpool, 1997 Recent Environmental United Kingdom. Change Bachelor of Fisheries Universiti Putra 1996 Marine science Sc. (Marine Sciences) Malaysia, Malaysia. 1 Diploma in Fisheries Universiti Putra 1993 Fisheries Malaysia, Malaysia. RESEARCH PROJECTS Project Project Title Role Year Funder Status No. B-08-0- Tidal effects on salinity Co- 2002-2003 FRGS Completed 12ER intrusion and suspended Researcher sediment discharged in Manggatal River Estuary, Sabah SCF0019- Study of the factors regulating Co- 2006 -2009 Science Completed AGR-2006 the bloom mechanisms of Researcher Fund harmful algal species in Sabah SCF0015- Coastal processes and Co- 2006 -2009 Science Completed ENV-2006 geomorphologic Researcher Fund characteristics of major coastal towns in East Sabah for assessment -
Public Health Ordinance, 1960
For Reference Only Subsidiary Legislation 1 of 2 No. S 37 PUBLIC HEALTH ORDINANCE, 1960 (Ordinance No. 7 of 1960) APPOINTMENT OF HEALTH OFFICERS (Section 4 (1)) In exercise of the powers conferred by subsection (1) of Section 4 of the Public Health Ordinance, 1960, I, the Director of Medical Services, Sabah, with the approval of the Minister has appointed the officers named in the first column herein as Health Officers in respect of the Administrative Districts set out opposite their names:- COLUMN I COLUMN II Officers Appointed Administrative Districts 1. Principal Medical Officer of Health, - Districts of Kota Kinabalu Kota Kinablu and Penampang. 2. Medical Officer in-charge, Papar - District of Papar. 3. Area Medical Officer of Health, - District of Tuaran Tuaran 4. Medical Officer in-charge, Kota - District of Kota Belud. Belud 5. Medical Officer in-charge, Ranau - District of Ranau. 6. Area Medical Officer of Health, - Districts of Sandakan and Sandakan Kinabatangan. 7. Medical Officer in-charge, - District of Labuk/Sugut Labuk/Sugut (Beluran) (Beluran). 8. Area Medical Officer of Health, - Districts of Tawau and Tawau Kunak. 9. Medical Officer in-charge, Semporna - District of Semporna. 10. Medical Superintendent, Lahad Datu - District of Lahad Datu. 11. Area Medical Officer of Health, - Districts of Keningau and Keningau Nabawan/Pensiangan. 12. Medical Superintendent, Tenom - District of Tenom. 13. Medical Officer in-charge, Tambunan - District of Tambunan. Public Health (Appointment of Health Officers) For Reference Only Subsidiary Legislation 2 of 2 14. Area Medical Officer of Beaufort - Districts of Beaufort, Kuala Penyu and Sipitang. 15. Area Medical Officer of Health, - Districts of Kudat, Kota Kudat Marudu and Pitas. -
Occurrences of Red Tide in Brunei Darussalam and Methods of Monitoring and Surveillance
Occurrences of Red Tide in Brunei Darussalam and Methods of Monitoring and Surveillance Matdanan Haji Jaafar and Selvanathan Subramaniam Fisheries Department, Brunei Darussalam Introduction Red Tide Occurrence in 1976 Negara Brunei Darussalam is situated in the On 11 March 1976, Fisheries Department northwest of Borneo Island and lies between biologists were conducting unrelated work at sea Sarawak to the southwest and Sabah to the when they noticed an extensive reddish-brown northeast. It lies between latitudes 4°N and 5° 05’ N discolouration 4 nautical miles north-northeast of and longitudes 114° 04’E and 115° 22’E. Muara Port. This was suspected as being a To the northeast of Brunei Darussalam, lies planktonic bloom and samples were collected. Brunei Bay and Brunei River estuary. These are Subsequent microscopic examination of the fringed by mangroves and form the basis of an samples showed the presence of heavy important prawn and seasonal Rastrelliger fishery. concentrations of a marine dinoflagellate that was The deep channel entering the bay between later identified as Pyrodinium bahamense Plate Pulau Muara Besar and Tanjong Trusan and the (1906). Although red tide was unknown in Brunei at dredged areas in the Muara Port area are relatively that time, its potentially toxic nature when deep but generally the water in the inner bay area concentrated was recognized and the Director of varies between 2 and 6 m. Fine sands, silts, and Medical Services was advised of the situation. A muds with a high organic content comprise the statement warning the public not to eat shellfish was sediment. Salinity in the bay varies from 15—28 ppt, broadcast over the radio and television the same but this fluctuates depending on tidal activity and evening. -
9. Archreolo~Ical Research in North Borneo*
9. Archreolo~ical Research in North Borneo* THOMAS RHYS WILLIAMS No systematic prehistoric research has been conducted to date in North Borneo. However, a variety of miscellaneous artifactual materials have come from this area, for over a half century, out of any stratigraphic context. Several random collections or prehistoric materials were made by officers of the North Borneo Chartered Company, but generally were destroyed in World War II, or now are scattered widely in England, Australia and elsewhere. Some items, randomly collected, are now in collections of the Sarawak Museum. These collections have been used to reconstruct North Borneo prehistory; but the chronologies and relationships suggested so far are no more than highly general speculations. Prehistoric cultural sequences, relationships, and specific chronologies, as determined by comparative geological, palreontological, stratigraphic and typological evidences, remain to be established by specific investigations based on the techniques and logical processes ofmodern science. Studies of a scientific nature will have to be conducted by visiting scholars until there are trained archreologists resident in the country. This report is intendedto drawattentionto sites likelytobeproductiveofsignificantprehistoricdata. In the course of ethnological study of the Dusun in 1959-60, and 1962-63 I took opportunity to survey four cave sites which appeared to offer possibilities for systematic archreological research. One large cave site, located in a limestone formation near Batu Punggul, on the Sungei Palagan, in the Pensiangan district of the North Borneo Interior Residency o (approximately 4!O N. I 16i E.), seems at the moment to hold greatest promise of prehistoric materials in sequence of time and association. -
Incision of Rivers in Pleistocene Gravel and Conglomeratic Terraces: Further Circumstantial Evidence for the Uplift of Borneo During the Neogene and Quaternary
Bulletin of the Geological Society of Malaysia, Volume 61, December 2015, pp. 49 – 57 Incision of rivers in Pleistocene gravel and conglomeratic terraces: Further circumstantial evidence for the uplift of Borneo during the Neogene and Quaternary FRANZ L. KESSLER1* & JOHN JONG2 1Independent Geoscience, Oil and Gas Consultant 2JX Nippon Oil and Gas Exploration (Deepwater Sabah) Limited Level 51, Menara 3 PETRONAS, Persiaran KLCC, Kuala Lumpur City Centre, 50088 Kuala Lumpur *Corresponding author: [email protected] Abstract: Incised Pleistocene gravel beds and conglomerates are a common feature of the Baram, Limbang and Temburong drainage systems in NW Sarawak and Brunei. Incision values vary from 9 to 76 m, a likely result of strong temporary precipitation, in combination with ongoing uplift. Conglomerates and gravels are monomictic, almost exclusively formed by the Lower Miocene Meligan sandstone, and deposited in nested fluvial terraces. The described pattern differs from coastal terraces of the Miri area; the latter do not contain conglomerates other than locally-derived and recycled quartz clasts. The available age and uplift data, when plotted log-normal, suggest that the mountainous central Borneo uplift was continuous of some 6-7 mm a-1, whilst low-lying coastal wetland areas in Brunei and Sarawak may only have seen a very minor uplift in the order of 0.8 mm a-1. The uplift may be ongoing at the present day. Keywords: NW Borneo, Neogene, Quaternary, terraces, uplift, Sarawak, Brunei, geomorphology INTRODUCTION research poses the question, to which extent climate may This paper is in many ways a compilation, given there have prompted the rise the Borneo hinterlands, as well as is a need to align older data with modern results, and mountainous regions of Sulawesi, New Guinea and other from different branches of science. -
Brunei Darussalam's Preliminary Submission Concerning the Outer
Brunei Darussalam’s Preliminary Submission concerning the Outer Limits of its Continental Shelf Brunei Darussalam’s Preliminary Submission to the Secretary-General concerning the Outer Limits of its Continental Shelf 1. Introduction (a) Relevant Provisions of UNCLOS 1. Brunei Darussalam (‘Brunei’) is a State party to the 1982 United Nations Convention on the Law of the Sea (‘UNCLOS’), which it signed on 5 December 1984 and ratified on 5 November 1996. 2. Article 77, paragraphs 1 – 3, of UNCLOS provide that: “1. The coastal State exercises over the continental shelf sovereign rights for the purpose of exploring it and exploiting its natural resources. 2. The rights referred to in paragraph 1 are exclusive in the sense that if the coastal State does not explore the continental shelf or exploit its natural resources, no one may undertake these activities without the express consent of the coastal State. 3. The rights of the coastal State over the continental shelf do not depend on occupation, effective or notional, or on any express proclamation.” 3. Article 76, paragraph 1, of UNCLOS establishes the right of coastal States to determine the outer limits of the continental shelf. This provision states that: “The continental shelf of a coastal State comprises the sea-bed and subsoil of the submarine areas that extend beyond its territorial sea throughout the natural prolongation of its land territory to the outer edge of the continental margin, or to a distance of 200 nautical miles from the baselines from which the breadth of the territorial sea is measured where the outer edge of the continental margin does not extend up to that distance.” Article 76, paragraph 8, of UNCLOS further states that: “Information on the limits of the continental shelf beyond 200 nautical miles from the baselines from which the breadth of the territorial sea is measured shall be submitted by the coastal State to the Commission on the Limits of the Continental Shelf set up under Annex II on the basis of equitable geographic representation. -
Maritime Briefing
International Boundaries Research Unit MARITIME BRIEFING Volume 1 Number 3 The Brunei-Malaysia Dispute over Territorial and Maritime Claims in International Law Renate Haller-Trost Maritime Briefing Volume 1 Number 3 ISBN 1-897643-07-1 1994 The Brunei-Malaysia Dispute over Territorial and Maritime Claims in International Law by R. Haller-Trost Edited by Clive Schofield and Martin Pratt International Boundaries Research Unit Department of Geography University of Durham South Road Durham DH1 3LE UK Tel: UK + 44 (0) 191 334 1961 Fax: UK +44 (0) 191 334 1962 e-mail: [email protected] www: http://www-ibru.dur.ac.uk The Author R. Haller-Trost holds a B.A. (Hons) in Anthropology, Southeast Asian Studies and Law from the University of Kent at Canterbury, UK. She is presently writing a PhD in International Law at Monash University, Melbourne, Australia. Her research interests are mainly the territorial and maritime disputes of Southeast Asia, a topic on which she has published various papers (e.g the Spratly Islands, Sabah, Brunei). NB: The opinions and comments contained herein are those of the author and are not to be construed as those of IBRU. Contents 1. Introduction 1 2. Brunei's Maritime Maps 2 3. Brunei's Territorial Land Claims 5 3.1 UK/Brunei Treaties after 1888 6 3.2 The Origin of the Claims 9 3.2.1 The Limbang and Rangau 11 3.2.2 The Trusan and Lawas 16 3.2.3 The Transfer of Sarawak in 1946 and 1963 19 3.3 Legal Assessment 20 3.3.1 Change of Sovereignty and Tenure 22 3.3.2 Alienation of Territory 23 3.3.3 Protectorates 24 3.3.4 Geographical Extent of the Limbang 26 3.3.5 Annexation 27 3.3.6 Uti Possidetis Iuris 31 3.3.7 Brunei Bay 33 4. -
INDIGENOUS GROUPS of SABAH: an Annotated Bibliography of Linguistic and Anthropological Sources
INDIGENOUS GROUPS OF SABAH: An Annotated Bibliography of Linguistic and Anthropological Sources Part 1: Authors Compiled by Hans J. B. Combrink, Craig Soderberg, Michael E. Boutin, and Alanna Y. Boutin SIL International SIL e-Books 7 ©2008 SIL International Library of Congress Catalog Number: 2008932444 ISBN: 978-155671-218-0 Fair Use Policy Books published in the SIL e-Books series are intended for scholarly research and educational use. You may make copies of these publications for research or instructional purposes (under fair use guidelines) free of charge and without further permission. Republication or commercial use of SILEB or the documents contained therein is expressly prohibited without the written consent of the copyright holder(s). Series Editor Mary Ruth Wise Volume Editor Mae Zook Compositor Mae Zook The 1st edition was published in 1984 as the Sabah Museum Monograph, No. 1. nd The 2 edition was published in 1986 as the Sabah Museum Monograph, No. 1, Part 2. The revised and updated edition was published in 2006 in two volumes by the Malaysia Branch of SIL International in cooperation with the Govt. of the State of Sabah, Malaysia. This 2008 edition is published by SIL International in single column format that preserves the pagination of the 2006 print edition as much as possible. Printed copies of Indigenous groups of Sabah: An annotated bibliography of linguistic and anthropological sources ©2006, ISSN 1511-6964 may be obtained from The Sabah Museum Handicraft Shop Main Building Sabah Museum Complex, Kota Kinabalu, Sabah, -
Malaysia and Brunei: an Analysis of Their Claims in the South China Sea J
A CNA Occasional Paper Malaysia and Brunei: An Analysis of their Claims in the South China Sea J. Ashley Roach With a Foreword by CNA Senior Fellow Michael McDevitt August 2014 Unlimited distribution Cleared for public release This document contains the best opinion of the authors at the time of issue. It does not necessarily represent the opinion of the sponsor. Cover Photo: South China Sea Claims and Agreements. Source: U.S. Department of Defense’s Annual Report on China to Congress, 2012. Distribution Distribution unlimited. Specific authority contracting number: E13PC00009. Copyright © 2014 CNA This work was created in the performance of Contract Number 2013-9114. Any copyright in this work is subject to the Government's Unlimited Rights license as defined in FAR 52-227.14. The reproduction of this work for commercial purposes is strictly prohibited. Nongovernmental users may copy and distribute this document in any medium, either commercially or noncommercially, provided that this copyright notice is reproduced in all copies. Nongovernmental users may not use technical measures to obstruct or control the reading or further copying of the copies they make or distribute. Nongovernmental users may not accept compensation of any manner in exchange for copies. All other rights reserved. This project was made possible by a generous grant from the Smith Richardson Foundation Approved by: August 2014 Ken E. Gause, Director International Affairs Group Center for Strategic Studies Copyright © 2014 CNA Foreword This is the second of three legal analyses commissioned as part of a project entitled, “U.S. Policy Options in the South China Sea.” The objective in asking experienced U.S international lawyers, such as Captain J. -
Report of the Second Workshop on the Biology and Conservation of Small Cetaceans and Dugongs of South-East Asia
CMS Technical Series Publication Nº 9 Report of the Second Workshop on The Biology and Conservation of Small Cetaceans and Dugongs of South-East Asia Edited by W. F. Perrin, R. R. Reeves, M. L. L. Dolar, T. A. Jefferson, H. Marsh, J. Y. Wang and J. Estacion Convention on Migratory Species REPORT OF THE SECOND WORKSHOP ON THE BIOLOGY AND CONSERVATION OF SMALL CETACEANS AND DUGONGS OF SOUTHEAST ASIA Silliman University, Dumaguete City, Philippines 24-26 July, 2002 Edited by W. F. Perrin, R. R. Reeves, M. L. L. Dolar, T. A. Jefferson, H. Marsh, J. Y. Wang and J. Estacion Workshop sponsored by Convention on Migratory Species of Wild Animals; additional support provided by Ocean Park Conservation Foundation, WWF-US and WWF-Philippines. Published by the UNEP/CMS Secretariat Report of the Second Workshop on the Biology and Conservation of Small Cetaceans and Dugongs of South-East Asia UNEP/CMS Secretariat, Bonn, Germany, 161 pages CMS Technical Series Publication No. 9 Edited by: W.F. Perrin, R.R. Reeves, M.L.L. Dolar, T.A. Jefferson, H. Marsh, J.Y. Wang and J. Estacion Cover illustration: digital artwork by Jose T. Badelles from a photograph by Jose Ma. Lorenzo Tan © UNEP/CMS Secretariat 2005 This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder, provided acknowledgement of the source is made. UNEP/CMS would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or for any other commercial purpose whatsoever with- out prior permission in writing from the UNEP/CMS Secretariat.