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.
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