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WARTA GEOLOGI NEWSLETTER of the GEOLOGICAL SOCIETY of MALAYSIA

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WARTA GEOLOGI NEWSLETTER of the GEOLOGICAL SOCIETY of MALAYSIA PERSATUAN GEOLOGI MALAYSIA WARTA GEOLOGI NEWSLETTER of the GEOLOGICAL SOCIETY OF MALAYSIA Jilid 38 APRIL–JUNE Volume 38 No. 2 2012 No. 2 ISSN 0126 - 5539 PP2509/07/2012(030291) Warta Cover 38_2.indd 1 7/16/2012 12:47:24 PM Warta Geologi Newsletter of the Geological Society of Malaysia PERSATUAN GEOLOGI MALAYSIA Editor-in-Chief Geological Society of Malaysia Ng Tham Fatt (University of Malaya) Council 2012/2013 Managing Editor President : Prof. Dr. Joy Jacqueline Pereira Ralph L. Kugler (University of Malaya) Vice President : Dr. Mazlan Madon Editorial Board Secretary : Mr. Ling Nan Ley Prof. Dr. Abdul Rahim Samsudin Assistant Secretary : Mr. Lim Choun Sian (Universiti Kebangsaan Malaysia) Treasurer : Mr. Ahmad Nizam Hasan Prof. Dr. Azman A. Ghani (University of Malaya) Editor : Assoc. Prof. Dr. Ng Tham Fatt Prof. Dr. Basir Jasin Immediate Past President : Dato’ Yunus Abdul Razak (Universiti Kebangsaan Malaysia) Councillors : Dr. Gan Lay Chin Assoc. Prof. Dr. Chow Weng Sum Dr. Liaw Kim Kiat (Universiti Teknologi Petronas) Dr. Meor Hakif Amir Hassan Prof. Dr. Felix Tongkul Mr. Nicholas Jacob (Universiti Malaysia Sabah) Dr. Nur Iskandar Taib Prof. Emeritus Dr. H.D. Tjia Mr. Robert Wong (Universiti Kebangsaan Malaysia) Mr. Tan Boon Kong Prof. Dato' Dr. Ibrahim Komoo Dr. Tanot Unjah (Universiti Kebangsaan Malaysia) Prof. Dr. J.J. Pereira (Universiti Kebangsaan Malaysia) Prof. Dr. John K. Raj The Geological Society of Malaysia was founded in (University of Malaya) 1967 with the aim of promoting the advancement of Prof. Dr. Lee Chai Peng geoscience, particularly in Malaysia and Southeast (University of Malaya) Asia. The Society has a membership of about 600 Prof. Dr. Mohd Shafeea Leman local and international geoscientists. (Universiti Kebangsaan Malaysia) Warta Geologi (Newsletter of the Geological Mr. Tan Boon Kong Society of Malaysia) is published quarterly by the (Consultant) Society. Warta Geologi covers short geological Prof. Dr. Teh Guan Hoe communications and original research, as well as (Consultant) reports on activities and news about the Society. It is distributed free-of-charge to members of the Prof. Dr. Wan Hasiah Abdullah Society. Further information can be obtained from: (University of Malaya) Dato' Yunus Abdul Razak The Editor (Minerals & Geoscience Department Geological Society of Malaysia c/o Department of Geology, Malaysia) University of Malaya, 50603 Kuala Lumpur, Malaysia Secretariat Tel: 603-79577036 Fax: 603-79563900 Anna Lim Email: [email protected] Cover photo: Colours and patterns of nature: Liesegang bands in sandstone, Belait Formation, Labuan by T.F. Ng Warta Cover 38_2.indd 2 7/16/2012 12:47:31 PM CATATAN GEOLOGI GEOLOGICAL NOTES Fosil moluska Trias Akhir dari kawasan Binjui, Kedah (Late Triassic molluscan fossils from Binjui area, Kedah) AHMAD ROSLI OTHMAN Jabatan Mineral dan Geosains Malaysia, Wisma Persekutuan, 15200 Kota Bharu, Kelantan Alamat emel: [email protected] Abstrak: Fosil ammonoid Frankites apertus (Mojsisovics), Zestoceras birwicki (Johnston), Anolcites anguinus Tozer dan Hungarites? sp. serta bivalvia Halobia charlyana Mojsisovics telah ditemui pada satu singkapan potongan jalan di kawasan Binjui berhampiran simpang Kejai-Binjui, Kedah. Fosil tersebut ditemui dalam lapisan syal dari Ahli Ridemit kepunyaan Formasi Semanggol yang berusia Perm Bawah hingga Trias Atas. Himpunan ammonoid ini mencirikan Subzon canadensis yang berusia Karnian Bawah (Trias Awal). Penemuan himpunan ammonoid ini dilaporkan buat pertama kalinya dalam Ahli Ridemit Formasi Semanggol dalam Zon Batuan Trias Barat, Semenanjung Malaysia. Abstract: Fossils ammonoids Frankites apertus (Mojsisovics), Zestoceras birwicki (Johnston), Anolcites anguinus Tozer and Hungarites? sp. and the bivalve Halobia charlyana Mojsisovics have been discovered at a road-cut in the vicinity of Binjui near the Kejai-Binjui road junction, Kedah. These fossils were found in a shale bed belonging to the Rhythmite Member the Lower Permian to Upper Triassic Semanggol Formation. This ammonoid assemblage is characteristic of the Lower Carnian (Upper Triassic) canadensis Subzone. The discovery of this ammonoid assemblage is reported for the first time in the Rhythmite Member of the Semanggol Formation within the Western Triassic Rock Zone of Peninsular Malaysia. Keywords: Ammonoid, Bivalve, Lower Carnian, Upper Triassic, Semanggol Formation PENGENALAN KERANGKA GEOLOGI Formasi Semanggol telah diperkenalkan oleh Kawasan kajian terletak dalam terain Sibumasu Alexander (1959) untuk batuan sedimen yang tersingkap dalam Jaluran Barat (Melcafe, 2000) dan berada dalam di kawasan Semanggol di utara Perak. Formasi ini Zon Batuan Trias Barat (Rajah 2) yang dicirikan oleh mengunjur melepasi sempadan Thailand di mana ia boleh kebersekutuan bivalvia Daonella, Halobia dan Peribositra dikorelasikan dengan Kumpulan Lampang. Formasi ini dalam lapisan syal (Kobayashi, 1963 & Kobayashi et dibahagikan kepada tiga ahli iaitu Ahli Rijang, Ahli al., 1966). Ridemit dan Ahli Konglomerat oleh Burton (1973). Kawasan kajian berada dalam Formasi Semanggol Ahli Rijang yang didominasi oleh turutan batuan rijang yang berjulat usia dari Perm Awal hingga Trias (Basir mempunyai fosil radiolaria yang berusia Perm hingga Jasin & Zaiton Harun, 2007). Formasi ini mempunyai Trias (Basir Jasin, 1997; Basir Jasin & Zaiton Harun, tiga unit batuan yang ditafsirkan bersentuhan secara 2007; Sashida et al., 1995). Ahli Ridemit pula mempunyai lateral dan berjejari antara satu sama lain iaitu Ahli fosil Daonella, Halobia dan Posidonia (=Peribositra) Ridemit, Ahli Konglomerat dan Ahli Rijang (Ahmad serta ammonoid yang berusia Trias Tengah hingga Trias Jantan et al., 1989; Basir Jasin et. al., 1989). Ahli Ridemit Akhir (Kobayashi et al., 1966). Formasi Semanggol ditafsirkan terenap di kawasan hujung Singkapan batuan Ahli Ridemit yang mempunyai fosil kipas samudera dalam (Ahmad Jantan et al., 1989) dan moluska bivalvia dan ammonoid telah ditemui di kawasan tersingkap dengan meluas di kawasan Gunung Semanggol Binjui, Kuala Ketil dalam Daerah Baling, Kedah (Rajah di utara Perak serta di bahagian selatan dan utara Kedah. 1). Kajian ini mendokumentasikan penemuan tersebut Di kawasan Baling, singkapan Ahli Ridemit boleh dilihat merangkumi pemerihalan fosil, kajian biostratigrafi, di sepanjang jalanraya yang menghubungkan Bandar korelasi dan penentuan usia fosil. Fosil ammonoid dalam Baling dan Bandar Sg. Petani. kajian ini adalah pertama kali dilaporkan dalam Ahli Litologi Ahli Ridemit terdiri daripada saling lapis batu Ridemit Formasi Semanggol dan dalam Zon Batuan Trias pasir dan syal atau batu lumpur dengan sedikit perlapisan Barat umumnya. atau kekanta konglomerat. Litologinya adalah menyerupai ISSN 0126–5539 Warta Geologi, Vol. 38, No. 2, Apr–Jun 2012, pp. 27–34 Warta 38_2.indd 27 7/18/2012 9:54:46 PM AHMAD ROSLI OTHMAN Rajah 1: Peta menunjukkan lokasi fosil dan geologi kawasan kajian. batuan klastik dalam Ahli Rijang. Batu pasirnya adalah berkomposisi greiwak litik yang mempamerkan perlapisan silang, lapisan tergred dan terlaminasi manakala syalnya berwarna kelabu cerah hingga kelabu gelap. Syal ini mengandungi banyak fosil bivalvia berusia Trias Tengah hingga Trias Akhir (Kobayashi et al., 1966). Halobia dan terutamanya Peribositra paling biasa ditemui dalam Ahli Ridemit dan Ahli Konglomerat (Kobayashi & Tamura, 1984). Menurut Kobayashi dan Tamura (1984), fosil bivalvia dalam Ahli Ridemit lazimya ditemui pada satah-satah perlapisan syal di mana cengkerangnya terawet dengan baik serta tidak mengalami canggaan. Fauna bivalvia dalam Ahli Ridemit didapati bersifat pelagik dan bercengkerang nipis yang didominasi oleh spesies-spesies dari genus Daonella, Halobia dan Posidonia termasuklah Daonella burtoni, D. cf. kotoi, D. pectinoides, D. indica, D. multilineata, D. posidoniformis, D. procteri, D. sumatrensis, Halobia aotii, H. cf. austriaca, H. cf. styiaca, H. cf. mollukana, H. charlyana, H. comata, H. aotii, H. paralella, H. subquadrata, H. talauna, Peribositra cf. cycoidalis, B. cf. idriana, B. cf. japonica, B. kedahensis dan B. tawarensis. Menurut Kobayashi et al. (1966), kehadiran Posidonia kedahensis, Halobia comata dan Halobia aotii menunjukan bahawa usia syal ini berjulat dari Karnian Awal hingga Norian Awal. Namun begitu penetapan julat Rajah 2: Peta menunjukkan kedudukan kawasan kajian usia berdasarkan bivalvia tersebut terlalu umum dan perlu yang terletak dalam Zon Batuan Trias Barat. Diubahsuai dari disokong oleh kehadiran fosil-fosil lain khasnya fosil Kobayashi et al. (1964). ammonoid. Fosil ammonoid memainkan peranan yang penting dalam membina biostratigrafi dan biokronologi Trias relatif terhadap usia geologi (Tozer, 1971;1994; Mietto & Manfrin, 1995; Lucas, 2010). 28 Warta Geologi, Vol. 38, No. 2, April – June 2012 Warta 38_2.indd 28 7/18/2012 9:54:47 PM FOSIL MOLUSKA TRIAS AKHIR DARI KAWASAN BINJUI, KEDAH SINGKAPAN BATUAN Lokaliti fosil yang dikaji adalah berkedudukan pada longitud 5°34.778’ U dan latitud 100°44.224’ T. Fosil moluska ditemui pada jujukan batuan berketebalan lima meter yang tersingkap pada satu cerun potongan jalan raya (Rajah 3) yang menghubungkan Bandar Baling dan Sg. Petani berhampiran simpang Kejai-Binjui. Terdapat tiga fasies batuan yang dicerap pada singkapan ini iaitu fasies batu pasir masif, batu pasir berlapisan silang dan selang lapis antara syal kelabu dengan syal kelabu gelap yang miring 30° ke arah tenggara. Fosil boleh ditemui dalam lapisan syal yang berkedudukan di bahagian bawah jujukan batuan seperti yang ditunjukkan dalam Rajah 3 dan
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