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Persatuan Geologi Malaysia

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Persatuan Geologi Malaysia ISSN 0126-5539 PERSATUAN GEOLOGI MALAYSIA NEWSLETTER OF THE GEOLOGICAL SOCIETY OF MALAYSIA KANDUNGAN (Contents) CATATAN GEOLOGI (Geological Notes) Azman Abdul Ghani: Occurrence of synplutonic dykes from Perhentian 65 Kecil Island, Besut, Terengganu H.D. Tjia: Eruptive or impact breccia? Bukit Lebam, Johor 69 PERTEMUAN PERSATUAN (Meetings of the Society) Annual General Meeting 1998 & Annual Dinner 1998 - Report 73 Minutes of the 31st Annual General Meeting (1996/97) 75 BERITA-BERITA PERSATUAN (News of the Society) Keahlian (Membership) 91 Pertukaran Alamat (Change of Address) 92 Pertambahan Baru Perpustakaan (New Library Additions) 92 Resignation of President and Vice President 93 Keputusan Peraduan Fotografi '97 93 BERITA-BERITA LAIN (Other News) Local News 99 Water Resources Management in Intermontane Basins 109 19th International Geochemical Exploration Symposium 111 Kalendar (Calendar) 112 Majlis (Council) 1998/99 Presiden (President) Ibrahim Komoo Naib Presiden (Vice-President) S. Paramananthan Setiausaha (Secretary) Ahmad Tajuddin Ibrahim Penolong Setiausaha (Asst. Secretary) Mazlan Madon Bendahari (Treasurer) Lee Chai Peng Pengarang (Editor) Teh Guan Hoe Presiden Yang Dahulu (Immediate Past President) : KhalidNgah Atili-Ahli Majlis;<~e()uniillors) 1998-2000 1998-1999 M. Selvarajah Azhar Hj. Hussin Abd. Ghani Mohd Rafek K.K. Liew Tajul Anuar Jamaluddin Kadderi Md. Desa Muhinder Singh Tan Boon Kong Jawatankuasa Kecil Pengarang (Editorial Subcommittee) Teh Guan Hoe (PengerusilChairman) Fan Ah Kwai Ng Tham Fatt J.J. Pereira Lembaga Penasihat Pengarang (Editorial Advisory Board) AwPeckChin Foo Wah Yang Mazlan Madon Tan Boon Kong Azhar Hj. Hussin C.A. Foss Ian Metcalfe Tan Teong Hing K.R. Chakraborty N.S. Haile S. Paramananthan Teoh Lay Hock Choo Mun Keong C.S. Hutchison Senathi Rajah H.D. Tjia Chu Leng Heng Lee Chai Peng Shu Yeoh Khoon Wan Hasiah Abd. Denis N.K. Tan Leong Lap Sau P .H. Stauffer Yeap Cheng Hock Aboutth.SoCiety The Society was founded in 1967 with the aim of promoting the advancement of earth sciences particularly in Malaysia and the Southeast Asian region. The Society has a membership of about 600 earth scientists interested in Malaysia and other Southeast Asian regions. The membership is worldwide in distribution. Published by the Geological Society of Malaysia, Department of Geology, University of Malaya, 50603 Kuala Lumpur. Tel: 603-757 7036 Fax: 603-756 3900 E-mail: [email protected] Printed by Art Printing Works Sdn. Bhd., 29 Jolon Rlong, 59100 Kuala Lumpur. Occurrence of synplutonic dykes from Perhentian Kecil Island, Besut, Terengganu AzMAN ABDUL GHANI Geology Department University of Malaya 50603 Kuala Lumpur Abstract: This short note reports field and microscopic observations of the synplutonic dykes from the Perhentian Kecil syenite. The observations suggest that the dykes were intruded when the host magma was partially crystallised. INTRODUCTION pegmatite (2 to 3 cm across) can be seen bordering and sometimes veining into the dyke During the mapping course of the (Fig. 2). Subhedral to anhedral syenitic Perhentian Island area, two synplutonic dykes inclusions with sizes that range from several were found intruding the Perhentian Kecil mm up to 2 cm across are scattered throughout syenite (SPK). The aim of this paper is to the dykes. The inclusions are either report the field characteristics ofthe synplutonic monomineralic (usually K-feldspar) or consist dykes and its implications. The Perhentian of a clot of several minerals (K-feldspar, Kecil syenite consists of a gradational sequence hornblende and plagioclase). Lobes of syenite of intermediate to mafic igneous rocks ranging material occasionally penetrated into the dykes in composition from syenitic to gabbroic. It resulting in lobate and cuspate contacts between formed a nearly circular shaped pluton and the dykes and the Perhentian Kecil syenite. has in turn been intruded by the Perhentian granite (GP). The contact between the two Detail inspection of sawn slabs of the dyke plutons can be seen at Pasir Patani, Tanjung from Tanjung Batu Jalil shows that the dyke Batu Nisan, Pasir Karang and Tanjung Batu is banded. It consists of alternating greyish Peti (Fig. 1). non-biotite and reddish grey biotite-bearing bands. In thin section the dykes show a FIELD AND MICROSCOPIC amphibolitic texture suggesting its basic origin. DESCRIPTIONS Flow texture of fine-grained hornblende and biotite are well-developed at the margin of the The dykes were found at two locations feldspar inclusion and dying out away from namely, (1) Tanjung Batu Peti and (2) Tanjung the inclusion. Batu Jalil (Fig. 1). They are more mafic and finer grained than the syenite host. Field sketch IMPLICATION of both dykes are shown in Figures 2 and 3 respectively. The dykes vary in width from a The field features shown by the dykes in few cm to 20 cm and lengths up to several the present study is similar to synplutonic dykes meters and are marked by necking and elsewhere (Roddick and Armstrong, 1959; disrupting or pinching and swelling along their Pitcher and Read, 1960; Pitcher and Bussell, lengths. At Tanjung Batu Peti, a K-feldspar 1985; Reid and Hamilton, 1987; Pitcher, 1991, ISSN 0126-5539 Warta Geologi, Vol. 24, No. 2, Mar-Apr 1998, pp. 65-68 LEGEND 0) IT] Syenite 0) loneous Susu Dora comPle, ~ Keeil a::J"\o,. Granite __,~ ~ ~ Rowa E3 ~O [2] Metasediment Susu Dora. / Undifferenciated mafic dyke Besar SOU T H CHI N A 5 E A N 0 2 I t km ~ Serenggeh 103 0 o I km .. 60 .. t· .... ".... , , ," , I \ , I I \ + + ( "1'""" .. ",,, .,-" \ , '. WEST '. , Perhentian 4" Pasir Besar + MALAYS IA ',' Karam~ , '. + + Pasir Patani Figure 1. Map of Pulau Perhentian and its surrounding area showing the location ofTanjung Batu Jalil and Tanjung Batu Peti on Perhentian Kecil, where both dykes described in the text occur. OCCURRENCE OF SYNPLUTONIC DYKES FROM PERHENTIAN KECIL ISLAND, BESUT 67 syenite host Hornblende K-feldspar pegmatite Hornblende 10em Figure 2. Field sketch of the dykes from Tanjung Batu Peti. syenitic vei n microgranite syenitic inclusion dyke o o / I / I syenitic host / I / / I / / " I " / o em 45 Figure 3. Field sketch of the dyke from Tanjung Batu Jalil. Warta Geologi, Vol. 24, No.2, Mar-Apr 1998 68 AzMAN ABDUL GHANI 1993). The implication of the occurrence of the partially crystallized Perhentian Kecil dykes are: syenite. (1) The field relation suggests that the dykes (2) The interaction between the Perhentian represent a mafic magma (basaltic) that Kecil syenite and the dykes can be further was injected into a more silicic magma investigated by using serial studies of (syenitic) chamber. thin sections and analytical techniques to establish if there are any chemical (2) Lobate to crenulate contact and necking diffusion gradients between these rocks. of the dykes suggest that the time of the dyke intrusion is coeval to its host (e.g. Pitcher, 1991; Vernon et al., 1988). The REFERENCES dykes probably were injected when the BUSSELL, M.A, 1991. Enclaves in the Mesozoic and syenitic magma was partially crystallised Cenozoic granitoids of the Peruvian Coastal and where both magmas were continuously batholith. In: J. Didier and B. Barbarin (Eds.), moving. Enclavesandgranitepetrology. Elsevier, 155-166. (3) The occurrence of syenitic inclusions in PITCHER, W.S., 1991. Synplutonic dykes and mafic the dykes suggests that the quenched enclaves. In: J. Didier and B. Barbarin (Eds.), dykes' carapaces were sometimes breached Enclaves and granite petrology. Elsevier, 383-391. by syenitic vein material which broke up PITCHER, W.S., 1993. The nature and origin ofgranite. into globules on penetrating the more fluid Blackie Academic, 321 p. interior of the dykes (Bussell, 1991). PITCHER, W.S. AND READ, H.H., 1960. Early tranverse (4) The amphibolitic texture of the dykes dykes in the Main Donegal granite. Geol. Mag., 97, suggests that they have undergone 53-61. metamorphism. The texture may also PITCHER. W.S. AND BUSSELL, M.A., 1985. Andean dyke have resulted from the metasomatic swarms: andesite in synplutonic relationship with process resulting from the differences in tonalite. In: W.S. Pitcher, M.P. Atherton., E.J. concentration gradients of certain elements Cobbing and R.D. Beckinsale (Eds.), Magmatism at between the dyke and the host interface. a plate edge: the Peruvian Andes. Blackie Glasgow, 93-101. REID, J.B. AND HAMILTON, M.A., 1987. Origin of Sierra FURTHER STUDY Nevadan granite: evidence from small scale composite dikes. Contrib. Mineral. Petrol., 96, 441- Suggestions for further study concerning 454. these dykes are: RoDDICK, J.A. AND ARMsTRONG, J.E., 1959. Relict dikes (1) The dykes probably provided some clues in the Coast Mountains near Vancouver, B.C. Jour. regarding the heat source of the igneous Geol., 67, 603-613. rocks from the area (namely, the VERNON, R.H., ETHERIDGE, M.A AND WAIL, V.J., 1988. Perhentian Kecil syenite) as it may Shape and microstructure of microgranitoid represent an offshoot of the underplated enclaves: indicators of magma mingling and flow. mafic magmas which intruded into the Lithos., 22, 1-11. ---------.~.-~~.-.-------- Manuscript received 7 November 1997 Warta Geologi, Vol. 24, No.2, Mar-Apr 1998 Eruptive or impact breccia? Bukit Lebam, Johor H.D. TJIA Petronas Research & Scientific Services Sdn. Bhd. Lots 3288 & 3289, Kawasan Institusi Bandar Baru Bangi 43000 Kajang, Selangor The small-scale geological map of Sheet This interpretation is based on the 132, Sungai Papan published by Ismail Ahmad observation that in active volcanic craters, (1984) and the regional geological map well-rounded, partly decomposed clasts (Geological Survey of Malaysia, 8th edition, of igneous rock occur side by side with 1985) show Bukit Lebam (104°12'30"E, fresh-looking, but angular blocks of the OP32'50"N) as a Permian, or Permo-Triassic, same material. patch of mainly felsic pyroclastics among 5. A black, sooty looking soft rock grades metasedimentary rocks of older age. The into mauve-coloured shale. The black pyroclastics may be correlated with the J asin colour probably indicates carbonaceous Volcanics of Suntharalingam (1981) or the material.
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