Готові списки джерел за темами / Peninsular Malaya

Добірка наукової літератури з теми "Peninsular Malaya"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 28 січня 2023

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Статті в журналах з теми "Peninsular Malaya"

1

LEOW, RACHEL. "‘Do you own non-Chinese mui tsai?’ Re-examining Race and Female Servitude in Malaya and Hong Kong, 1919–1939." Modern Asian Studies 46, no. 6 (March 12, 2012): 1736–63. http://dx.doi.org/10.1017/s0026749x1200011x.

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AbstractThis paper considers the abolition of the mui tsai (young female bondservants) as it unfolded in British Malaya, and challenges the overemphasis on Hong Kong as the primary focus of mui tsai scholarship. While the mui tsai system was defended as a time-honoured Chinese tradition, this paper uses new material to show that trans-racial considerations figured prominently in mui tsai abolition in Malaya, particularly in helping to recast it as a wider problem of child welfare. It is argued that this neglected aspect of mui tsai abolition only comes clearly to light in the Malayan case; for only in the intensely multi-racial conditions of peninsular Malaya could the question be asked: ‘Do you own non-Chinese mui tsai?’
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2

Julius, Avelinah. "Buxus holttumiana of Peninsular Malaysia and Thailand is a variety of B. cochinchinensis (Buxaceae)." Phytotaxa 167, no. 2 (May 9, 2014): 201. http://dx.doi.org/10.11646/phytotaxa.167.2.7.

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The Flora of Peninsular Malaysia project was initiated in 2005 (Kiew & Rafidah 2007, Saw & Chung 2007), and aims to document the entire flora of the region formerly known as Malaya or Malay Peninsula. As part of this project, the present author is revising the Buxaceae for the Flora, represented in Peninsular Malaysia by the single genus Buxus Linnaeus (1753: 983). The genus was last revised by Hatusima in 1942, and in his revision, Hatusima recognized three species in Peninsular Malaysia [viz. Buxus holttumiana Hatusima (1942: 270), B. malayana Ridley (1926: 475) and B. rupicola Ridley (1911: 166)]. All three taxa are confined to limestone forests at 20–450 m above sea level, and Hatusima (1942) considered all species as endemic to Peninsular Malaysia. In his revision, however, Hatusima described B. holttumiana from a single collection gathered in 1938 from Kaki Bukit, Perlis (Kiah SFN 35239, see Figure 1A & B) and considered the thicker, shining leaves with fewer veins, the longer, erect (not strongly recurved and divaricating) styles as diagnostic characters for this species. Hatusima (1942), however, stated that he did not compare his new taxon with material of B. cochinchinensis Pierre ex Gagnepain (1921: 481), and his description of the latter was more or less a verbatim transcription of Gagnepain’s (Gagnepain 1921).
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3

Johns, Anthony H. "Sufism in Southeast Asia: Reflections and Reconsiderations." Journal of Southeast Asian Studies 26, no. 1 (March 1995): 169–83. http://dx.doi.org/10.1017/s0022463400010560.

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In 1961 I published in this Journal a paper on the Islamization of peninsular and insular Southeast Asia. It was a paper I had presented to the first meeting of the conference of historians of Southeast Asia organized in January of that year at the University of Malaya in Singapore by the then Raffles Professor of History, K.G. Tregonning. It was a paper often referred to in discussions concerning the coming of Islam to the Malay world, and attracted its share of approbation and criticism.
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4

Mohamed, Haji, and Benito C. Tan. "A Checklist of Mosses of Peninsular Malaya and Singapore." Bryologist 91, no. 1 (1988): 24. http://dx.doi.org/10.2307/3242736.

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5

Metcalfe, I. "Stratigraphic and tectonic implications of Triassic conodonts from northwest Peninsular Malaysia." Geological Magazine 127, no. 6 (November 1990): 567–78. http://dx.doi.org/10.1017/s0016756800015454.

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AbstractThe Chuping Limestone of northwest Peninsular Malaysia, until recently considered entirely of Permian age, has yielded late Triassic (early Norian) conodonts. TheLimestone thus spans the time interval late Early Permian–Late Triassic and is in part equivalent to the Kodiang Limestone (Late Permian–Late Triassic) in Kedah andsimilar limestone sequences in south Thailand and north Sumatra. Early Late Triassic (Carnian) conodonts are also reported from pelagic limestones associated with bedded chertsof the Chert Member of the Semanggol Formation in Kedah. The Chert Member, previously considered of Middle Triassic age, is re-interpreted to represent Early, Middle and early Late Triassic deposition. The Triassic sedimentary rocks of the Malay Peninsula represent three distinct sedimentary regions: a stable shallow marine carbonate complex (ChupingLimestone, Kodiang Limestone), which forms part of an elongate carbonate platform on theSibumasu block; a deep water pelagic/turbidite basinal sequence (Semanggol Formation) which accumulated in either a foredeep basin or an intracratonic pull-apart basin related to strike-slip faulting; and a volcanic-sourced volcaniclastic basinal sequence on the East Malaya block (Semantan Formation and equivalents) which accumulated in either a forearc/intra-arc setting, or in a post-orogenic rift basin.
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6

Low, Yvonne. "Becoming professional artists in postwar Singapore and Malaya: Developments in art during a time of political transition." Journal of Southeast Asian Studies 46, no. 3 (September 14, 2015): 463–84. http://dx.doi.org/10.1017/s002246341500034x.

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This article aims to recover the background to the post-Second World War growth of local art activities, art education and the rise of the professional artist on the island of Singapore and peninsular Malaya. It examines how the transitional period spanning the dissolution of British colonialism and the establishment of two independent nations stimulated unique conditions for the development of local art education and created an amateur–professional artist divide. The promotion and support of fine arts and related activities were in tandem with nation-building strategies that sought to construct a common ‘Malayan’ culture and identity.
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7

Leary, John D. "Orang Asli contacts with the Malays, Portuguese and Dutch in Peninsular Malaya from 1400 to 1700." Asian Studies Review 18, no. 2 (November 1994): 89–104. http://dx.doi.org/10.1080/03147539408712999.

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8

SONE, MASATOSHI, IAN METCALFE, and MOHD SHAFEEA LEMAN. "Palaeobiogeographic implications of Middle Permian brachiopods from Johore (Peninsular Malaysia)." Geological Magazine 140, no. 5 (September 2003): 523–38. http://dx.doi.org/10.1017/s0016756803007854.

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A new Middle Permian locality in northern Johore, Peninsular Malaysia, yields a small-sized, but compositionally unique, brachiopod fauna consisting of eight species: Pseudoleptodus sp., Caricula cf. salebrosa Grant, Neochonetes (Nongtaia) aff. arabicus (Hudson & Sudbury), Karavankina sp., Transennatia cf. insculpta (Grant), Hustedia sp., Orthothetina sp., and martiniid indet. The first four genera are new records for Malaysia; in particular, the rare taxa Pseudoleptodus and Caricula characterize the fauna. The brachiopods occur together with the ammonoid Agathiceras sp., the nautiloid Foordiceras? sp., bivalves, and crinoid stems. The locality belongs to the East Malaya terrane of the Cathaysian biotic region, but some affinities to species of the Sibumasu province are recognized. The Malaysian forms of Pseudoleptodus, Caricula and Transennatia are similar to those of the Ratburi Limestone (southern Thailand). A Roadian–early Wordian age is interpreted for the Johore fauna. The similarity of brachiopods reported here with those from the Ratburi Limestone suggests that there was species interchange or one-way migration between shallow waters of East Malaya and Sibumasu across the main Palaeo-Tethys. The Tethyan seaway between the two terranes must have been narrower than previously interpreted by some authors to allow such faunal traffic during the Roadian–Wordian time period.
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9

STOCKWELL, A. J. "Britain and Brunei, 1945–1963: Imperial Retreat and Royal Ascendancy." Modern Asian Studies 38, no. 4 (October 2004): 785–819. http://dx.doi.org/10.1017/s0026749x04001271.

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An organizing principle of Britain's pre-war empire was collaboration with indigenous monarchies. Secure on their thrones, they legitimated British rule as well as assisting it in practical ways. While friendly princes were assets, however, uncooperative ones could be liabilities; they might obstruct attempts to exploit their resources or to modernize their governments. After the Second World War, British priorities and strategies changed. With their backs to the wall they switched from supporting princes to accommodating politicians. There was no obvious role for them in new nation-states and in many dependencies indigenous monarchies were swept aside by the onrush of nationalism. Yet in Malaya and Brunei they survived: the rulers of the peninsular Malay states did so by adjusting to political change, whereas the Sultan of Brunei flourished by preventing it.
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Harper, T. N. "The Politics of the Forest in Colonial Malaya." Modern Asian Studies 31, no. 1 (February 1997): 1–29. http://dx.doi.org/10.1017/s0026749x00016917.

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The notion that tribal peoples are destructive of the forest environment is not a new one. The political struggles that fostered it are only just beginning to engage the attention of historians. This essay is a preliminary exploration of the experience of the indigenous minorities—the Orang Asli—of peninsular Malaysia during the period of colonial rule. It examines their relationship to the society outside the forest. The politics of the forest it addresses are not narrowly environmental. Indeed, what follows is based on the assumption that the relationship of the aborigines to their environment was transformed, not so much by the changing ecological conditions of the forest as the colonial economy expanded, but by the changing political circumstances of the frontier as the Orang Asli were drawn into a widening orbit of relations with external powers. ‘Orang Asli’ means literally ‘original people’. It is a polite term that took on a legal status from the 1950s. Before then, in common parlance, the aborigines were ‘Sakai‘—a derogatory term synonymous with ‘slave’. The term Orang Asli encompasses three basic types of communities: the Negritos, nomadic hunters and gatherers of the northern forests; the Senoi —whose two main subdivisions, the Temiar and the Semai, together make up the larger part of the Orang Asli population of the central highlands, following more settled forms of swidden agriculture; and the proto-Malays of the south, fishermen and cultivators with a more similar economy to neighbouring Malays.1Their shared history has become an issue of great sensitivity in modern Malaysia, and Malaysian politicians have in recent years bitterly questioned the legitimacy of western criticism of the present circumstances of the Orang Asli. To explain why this is so, I want to examine the preoccupations of British administration during the period when it was trustee of the forests of the peninsula and directly responsible for the welfare of their inhabitants. Three themes dominate the discussion that follows.
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Дисертації з теми "Peninsular Malaya"

1

Nallakumar, Anm. "The management and conservation of fireflies in peninsular Malaya." Thesis, Imperial College London, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.402580.

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Yusof, N. M. Z. B. H. N. "Land tenure and land law reforms in peninsular Malaya." Thesis, University of Kent, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.234468.

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3

Abdullah, Mohamed Rusli. "Malaria and malaria control in Jeli Peninsular Malaysia." Thesis, University of Liverpool, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.266047.

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4

Madon, Mazlan B. Hj. "Tectonic evolution of the Malay and Penyu Basins, offshore Peninsular Malaysia." Thesis, University of Oxford, 1995. http://ora.ox.ac.uk/objects/uuid:f00a727d-8769-4ac8-88ab-35d8c662ea61.

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The Malay and Penya Basins, offshore Peninsular Malaysia, were formed during the early Oligocene as a result of regional dextral shear deformation caused by the indentation of India into Eurasia in the early Tertiary. Pre-existing basement inhomogeneities exerted a strong control on basin development. The Penyu Basin developed, initially, as isolated grabens and half-grabens at basement fault intersections, in response to roughly N-S extension. The major structures which include low-angle listric normal faults, pull-apart rhomb grabens and flower structures, suggest that "thin-skinned" crustal extension and strike-slip tectonics have played an important role in basin evolution. Basement faults in the Malay Basin are oblique (E-W trending) to the basin trend (NW-trending). The Basin developed by transtension of NW-trending sinistral shear zone, in which fault-bounded blocks rotate in response to the shear deformation, producing a series of E-trending half-graben depocentres. The Basins were subjected to transpressive inversion during the middle-late Miocene, as a result of rotation of the regional stress field, caused by progressive indentation of India into Eurasia. Subsidence analysis suggests that lithospheric stretching was the dominant process of basin formation. The high heat flows (85-100 mW m⁻²) are consistent with stretching factors, β, of 1.2 to 4.3. In the Malay Basin, uplift of the basin flanks preceeded subsidence during the rifting phase as a result of non-uniform stretching and lateral heat flow from the centre of the Basin. Both basins are undercompensated isostatically and characterised by low negative free-air gravity anomaly in the order of -20 mGal. Undercompensation suggests that the basins were formed, partly, by "thin-skinned" crustal extension which did not involve stretching of the subcrustal lithosphere.
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5

Francis, Larry Hicarian. "The 'gambus' lutes of the Malay world and their music in peninsular Malaysia." Thesis, Goldsmiths College (University of London), 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.415017.

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6

Lee, Ho-yin, and 李浩然. "The kampong house : architecture and culture of the Malay vernacular in Peninsular Malaysia." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1998. http://hdl.handle.net/10722/207573.

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Lee, Ho-yin. "The kampong house : architecture and culture of the Malay vernacular in Peninsular Malaysia /." Hong Kong : University of Hong Kong, 1998. http://sunzi.lib.hku.hk/hkuto/record.jsp?B19472626.

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8

Hj, Omar Abdul Razak. "Voluntary labour turnover in west Peninsular Malaysia : a comparison of the experiences of the Chinese, Indians and Malays." Thesis, University of Stirling, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.294008.

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9

Ismail, Nik Ahmad Hisham. "Perceptions of leadership amongst ethnic Malay pupils in residential secondary schools in peninsular Malaysia in the context of national development." Thesis, University College London (University of London), 1998. http://discovery.ucl.ac.uk/10020306/.

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This thesis examines the perceptions of ethnic Malay pupils in Residential Secondary Schools (RSS) towards leadership in Malaysia. The thesis begins with a discussion on the struggle for leadership in the case of a multi-ethnic society like Malaysia. The thesis examines the circumstances that led to ethnic Malays' struggle for survival' through the policies of education. The thesis acknowledges that the establishment of the RSS was part of the ethnic Malays' struggle for survival' and has since become an important source for ethnic Malay leadership in Malaysia. The research framework has been developed using the concepts of leadership and elitism. In this study, the government has acted as the catalyst for modernising the ethnic Malay community. Thus, the RSS, as a governmental institution, is considered as playing an important role in selecting pupils who are expected to become the future leaders in Malaysia. The major research questions are: (a) what are the perceptions of ethnic Malay pupils towards education?; (b) what is the selection process for ethnic Malay pupils into the RSS?; (c) how do the RSS operate?; (d) What are the perceptions of ethnic Malay pupils towards leadership? and; (e) what are the perceptions of ethnic Malay pupils towards leadership in Malaysia? The quantitative data are analysed using Statistical Package for Social Sciences (SPSS) and Chi-Square analysis. The results are presented using frequency tables and significant values for the hypothetical analysis. The qualitative data are analysed using categorization and comparison. The results are presented using frequency tables and rankings. In addition, documentary analysis is used to complement the results in this research. In general, the results of the study show that there are both similarities and differences in the perceptions of pupils towards the importance of education, leadership and in particular leadership in Malaysia. The results show that pupils are indifferent in their perceptions towards education. However, the study would suggest that the role of education for national development, especially for ethnic Malays, may reflect the objectives and aims of the government for future ethnic Malay leadership in Malaysia. The results also show that pupils' perceptions towards leadership in general and leadership in the context of Malaysia are different in terms of their SES, demographic area, and academic achievements. The study suggests that religion, culture and ethnicity are still important factors for leadership in Malaysia.
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10

Herbert, Vincent. "La circulation maritime dans le detroit de malacca et ses effets sur la cote occidentale de la peninsule malaise." Nantes, 1999. http://www.theses.fr/1999NANT3006.

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Le detroit de malacca est l'un des passages les plus frequentes au monde. La cote occidentale de la peninsule malaise, en relation avec les faits de circulation maritime de cette region, permet de realiser une analyse geographique d'un espace restreint, mais riche en acteurs et en paysages. L'etude considere le detroit de malacca comme un geosysteme, compose de trois systemes dominants. Le contexte economique regional et international dans lequel se situe ce detroit permet d'expliquer pourquoi et comment le trafic maritime dans cette region s'est developpe de facon spectaculaire. L'analyse du systeme du trafic maritime (qui inclut la circulation transversale) identifie les principaux utilisateurs du detroits. Enfin, le milieu physique est un facteur determinant et limite le choix des routes maritimes. Un premier axe de recherche met en relation la forte frequentation du detroit et ses effets sur les activites de la cote occidentale de la peninsule malaise : (industries portuaires, peche, aquaculture et tourisme). Le second axe se consacre aux moyens mis en oeuvre pour ameliorer la securite de la circulation maritime. Il nous a conduit a la creation d'un indice de risque de pollution marine. Apres avoir compare la part de cette pollution aux pollutions d'origine continentale et littorale, nous avons analyse la politique malaisienne de gestion (structure administrative, choix politiques, relations diplomatiques. . . ), pour savoir si celle-ci repondait aux problemes de pollution. En analysant les effets spatiaux du trafic maritime du detroit de malacca sur la cote occidentale de la peninsule malaise, cette these propose une methode d'analyse geographique applicable aux detroits, ou a d'autres espaces maritimes etroits
The strait of malacca is one of the busiest maritime passage in the world, and the western coast of the malay peninsula is connected to the maritime traffic of this region. Thus it provides a possible way to carry out a geographical analysis of a limited area and yet which is full of various landscapes and actors. The study looks upon the straits of malacca as a geosystem which is made up of three prevailing systems. The strait is situated in a regional and international economic background which can explain why and how the maritime traffic has expanded in such a spectacular way. An analysis of the maritime traffic (which includes the transverse movements) identifies the main users of this strait. Lastly, the physical environment is a determining and restricting factor for the choice of the sea routes. A first research line associates the important traffic of the strait with the effects noticed on the activities of the western coast of the malay peninsula : port industries, fishing, aquafarming and tourism. The second line is dedicated to the means used to improve the maritime traffic security. It has led us to create a rating for the risk of maritime pollution. After the comparison between the share of this pollution and those of continental and coastal origins, we have analysed the malaysian government management policy (administrative structures, political choices, diplomatic relationships. . . ) to see if it corresponded to the pollution issues. By analysing the spatial effects of the strait of malacca maritime traffic on the western coast of the malay peninsula, this thesis intends to give a method of geographical analysis wich can be applied to straits as well as to narrow maritime area
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Книги з теми "Peninsular Malaya"

1

D, Round Philip, and Treesucon Uthai, eds. The birds of the Thai-Malay Peninsula: Covering Burma and Thailand south of the eleventh parallel, Peninsular Malaysia and Singapore. San Diego: Academic Press, 1999.

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2

Kleingrothe, C. J. Malay Peninsula: Straits Settlements & Federated Malay States. Kuala Lumpur: Jugra Publications, 2009.

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3

History of the Malay Kingdom of Patani. Athens, Ohio: Ohio University, Center for International Studies, 1985.

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4

Out east in the Malay Peninsula. Petaling Jaya: Fajar Bakti, 1991.

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5

Corbet, A. Steven. The butterflies of the Malay Peninsula. 4th ed. Kuala Lumpur, Malaysia: Malayan Nature Society, 1992.

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6

Ng, F. S. P. Endemic trees of the Malay Peninsula. Kuala Lumpur: Forest Research Institute Malaysia, 1990.

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7

der, Putten Jan van, and Kilcline Cody Mary 1961-, eds. Lost times and untold tales from the Malay world. Singapore: NUS Press, 2009.

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8

Women and party politics in Peninsular Malaysia. Singapore: Oxford University Press, 1987.

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9

Din, Anwar. Asas kebudayaan dan kesenian Melayu. Bangi: Penerbit Universiti Kebangsaan Malaysia, 2007.

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10

Mahmud, Zaharah. Traditional landscapes of the Malays of the Peninsula. Tanjong Malim, Perak Darul Ridzuan, Malaysia: Universiti Pendidikan Sultan Idris, 2004.

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Частини книг з теми "Peninsular Malaya"

1

Feaver, George. "Malay Peninsula." In The Webbs in Asia, 176–88. London: Palgrave Macmillan UK, 1992. http://dx.doi.org/10.1007/978-1-349-12328-5_6.

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2

Dick, Howard, and Peter J. Rimmer. "Peninsulas: Malaya and Annam." In Cities, Transport and Communications, 186–216. London: Palgrave Macmillan UK, 2003. http://dx.doi.org/10.1057/9780230599949_6.

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3

Wiryomartono, Bagoes. "Urbanism, Society, and Culture in the Malay Peninsular World: Bandar Malacca." In Livability and Sustainability of Urbanism, 205–38. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-8972-6_9.

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4

Malhi, Amrita. "‘We Hope to Raise the Bendera Stambul’." In From Anatolia to Aceh. British Academy, 2015. http://dx.doi.org/10.5871/bacad/9780197265819.003.0010.

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In the decades between the 1870s and the 1920s, groups of Malay Muslims circulated symbols of the Ottoman Caliphate in gestures of defiance against British colonial intervention on the Malay peninsula. This was the period of ‘forward movement’, in which Britain progressively colonised successive Malay States, and it roughly coincided with the European confrontations which produced the First World War, Ottoman collapse, and the abolition of the Caliphate. At peninsular and global scales, these developments advanced the geo-body as the only legitimate means by which to organise territory. As a result, the Muslim world located around the Indian Ocean was decisively divided into a series of discrete, contiguous states, fragmenting the ummah, its latent political community. Malayan invocations of the Caliphate were local responses to this global reorganisation, of which peninsular colonisation formed an important and disruptive part.
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"Preliminary Material." In The Malay Peninsula, i—xxxvii. BRILL, 2002. http://dx.doi.org/10.1163/9789047400684_001.

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"Introduction." In The Malay Peninsula, 1–2. BRILL, 2002. http://dx.doi.org/10.1163/9789047400684_002.

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"The Impact of Geology, Relief and Climate on the Historic Destiny of the Malay Peninsula." In The Malay Peninsula, 3–22. BRILL, 2002. http://dx.doi.org/10.1163/9789047400684_003.

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"The Role of the Malay Peninsula: Obstacle or Source of Contacts and Profit Among the Asian Civilizations?" In The Malay Peninsula, 23–71. BRILL, 2002. http://dx.doi.org/10.1163/9789047400684_004.

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"Contacts Between the Indian Subcontinent and the Malay Peninsula Before Indianization." In The Malay Peninsula, 73–93. BRILL, 2002. http://dx.doi.org/10.1163/9789047400684_005.

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"The First Accounts of Indianization in the Malay Peninsula." In The Malay Peninsula, 95–105. BRILL, 2002. http://dx.doi.org/10.1163/9789047400684_006.

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Тези доповідей конференцій з теми "Peninsular Malaya"

1

Roselee, Muhammad Hatta, Mohd Rozi Umor, Azman Abdul Ghani, Muhamad Hafifi Badruldin, and Long Xiang Quek. "Petrographic and geochemical characteristic of volcanic rocks from Tasik Kenyir and Kampung Awah, East Malaya block, Peninsular Malaysia." In THE 2017 UKM FST POSTGRADUATE COLLOQUIUM: Proceedings of the University Kebangsaan Malaysia, Faculty of Science and Technology 2017 Postgraduate Colloquium. Author(s), 2018. http://dx.doi.org/10.1063/1.5027948.

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2

Madon, M. "The Overpressure History of the Malay Basin, Offshore Peninsular Malaysia." In PGCE 2004. European Association of Geoscientists & Engineers, 2004. http://dx.doi.org/10.3997/2214-4609-pdb.259.6.

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3

Anwar, M. R., M. A. Fazil, N. Pendkar, J. J. B. Mohd Idris, A. S. Bt Arshad, and J. Zhou. "Potential Lower Synrift Reservoir in Eastern Flank of Malay Basin, Offshore Peninsular Malaysia." In Asia Petroleum Geoscience Conference and Exhibition (APGCE). European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202270198.

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4

Ng, Cia Yik, Wan Zurina Wan Jaafar, Faridah Othman, Sai Hin Lai, Yiwen Mei, and Juneng Liew. "Evaluation of Drought Conditions in Peninsular Malaysia during 1989-2018 using SPI and EDDI." In International Technical Postgraduate Conference 2022. AIJR Publisher, 2022. http://dx.doi.org/10.21467/proceedings.141.1.

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Droughts are constantly threatening the global water availability and food securities worldwide. This study aims to evaluate the short- and long-term (1-, 6- and 12-month) drought conditions in Peninsular Malaysia during 1989-2018 using Standardized Precipitation Index and Evaporative Demand Drought Index. Historical trends of drought conditions were analyzed using modified Mann-Kendall test. Spearman’s ρ approach was also applied to examine the spatial patterns of correlations between these drought indices. Based on the findings, Evaporative Demand Drought Index shows increasing tendency towards drier conditions in the northern half of Peninsular Malaysia, but opposite trends are observed for Standardized Precipitation Index. The time series of Evaporative Demand Drought Index are generally well-correlated to that of Standardized Precipitation Index at all three timescales for the whole study area, except for the northern region. The evidence presented suggests Evaporative Demand Drought Index is a great alternative for drought monitoring applications in Peninsular Malaysia.
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5

Satti*, Iftikhar Ahmed, Deva Ghosh, and Wan Ismail Wan Yusoff. "Integrated Seismic Interpretation, Offshore Peninsular Malaysia." In International Geophysical Conference, Qingdao, China, 17-20 April 2017. Society of Exploration Geophysicists and Chinese Petroleum Society, 2017. http://dx.doi.org/10.1190/igc2017-074.

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6

Roslan, R., J. Zhou, M. R. Anuar, R. Danial, S. N. A. Sy Khastudin, and N. A. A. Gapar. "RESERVOIR PROSPECTIVITY OF OLIGOCENE SYN-RIFT; CASE STUDY IN NORTH EAST MALAY BASIN, OFFSHORE PENINSULAR MALAYSIA." In APGCE 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201903405.

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7

Anuar, Azlina, M. Jamaal Hoesni, and Mansor Ahmad and Norhafizah Mohamed. "Hydrocarbon Generation and Inorganic Modeling of Carbon Dioxide Generation and Expulsion in The Malay Basin, Peninsular Malaysia." In PGCE 2006. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609-pdb.256.r17.

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8

Wei, B. H., N. M. Nor, M. R. Aripin, S. S. W. Sy Khairulmunir Wafa, K. H. Khalid, N. N. Nasaruddin, N. N. Mohd Shukri, N. F. Zawri, and J. Baharom. "Unleashing Potential Stratigraphic Play via High Resolution Strata-Slicing Approach in North Malay Basin, Offshore Peninsular Malaysia." In Asia Petroleum Geoscience Conference and Exhibition (APGCE). European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202270075.

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9

Kadir, Masran, Muhammad Ruzwin Rusli, Bukhari Samsudin, Saim Rahman, Sheereen Norizan, Thierry Wee, M. Alham M. Johan, et al. "First Successful Installation of Through-Tubing Ceramic Sand Screen in Seligi Oil Field, Offshore Peninsular Malaysia." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21440-ms.

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AbstractThe Seligi field, located 240 kilometers offshore peninsular Malaysia in the Malay basin was discovered in May 1971 and is one of the largest oil fields in Malaysia. Sand production in the Seligi field has been observed, especially from the J reservoirs group. Within the Seligi field, Well G was identified as one of the wells with sand production to surface that could lead to sand accumulation at surface facilities and erosion of equipment. Historically, there had been no in-situ sand control measures in the well. The default practice for sand control was to choke back the well, to prevent triggering of the surface sand probe (production with maximum sand-free rate). This approach however is a compromise, while it limits sand production, it also limits the production potential of the well (well technical potential). As part of the production enhancement assessment program, remedial sand-control methods were considered to increase the oil production while minimising sand production. Among the options considered was ceramic downhole sand screen installation. Ceramics have been used in many extreme erosion and corrosion applications, with ceramic sintered silicon carbide being 50 times harder than steel. Ceramic sand screens made with sintered silicon carbide offer much higher erosional resistance at speeds of 300ft/s sand impingement velocity. Due to the aggressive nature of the sands and high velocities of greater than 50ft/s in Well G, a through-tubing ceramic sand screen was selected. The ceramic sand screen served as a fit for purpose solution that allowed the well potential to be fully maximised, enabling a continuous production with minimal sand production at surface.This paper reviews the first successful pilot installation of through-tubing ceramic sand screen in Well G in the Seligi Oil Field, Offshore Peninsular Malaysia. Discussed are careful analysis and planning, i.e. velocity calculations, tool deployment simulations, tool inspections and detailed job procedure leading to a successful installation. With the ceramic sand screen installed, the well was able to produce at 100% production choke opening with lower tubing head pressure and has not produced sand at surface despite multiple shutdowns and well bean ups. The installation has also removed the need to have sand handling facilities at topside and has generated an implicated cost saving from expensive intervention programs. Given the success of this pilot installation, a baseline in sand control has been set for this field, with new well candidates being considered for future replication.
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Mohd-Arrabe', A. B., and Talip Noraini Noraini. "Pollen morphology of Rhizophora L. in Peninsular Malaysia." In THE 2013 UKM FST POSTGRADUATE COLLOQUIUM: Proceedings of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology 2013 Postgraduate Colloquium. AIP Publishing LLC, 2013. http://dx.doi.org/10.1063/1.4858687.

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