Paleozoic to Cenozoic sedimentary bedrock geology and lithostratigraphy of Singapore Thomas J.H. Dodd*¹, Martin R. Gillespie1, A. Graham Leslie1, Timothy I. Kearsey¹, Rhian S. Kendall2, Thomas P. Bide3, Marcus R. Dobbs3, Ian L. Millar3, Michael Kim Woon Lee4, Kiefer Chiam5 and Michael Goay5 1British Geological Survey, Lyell Centre, Research Avenue South, Edinburgh, EH14 4AP, United Kingdom. 2British Geological Survey, Cardiff University, Main Building, Park Place, Cardiff, CF10 3AT, United Kingdom. 3British Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG, United Kingdom. 4Neptune Court, 8 Marine Vista #15-33, Singapore 449032. 5BCA Academy, 200 Braddell Rd, Singapore 579700 *(Corresponding author email:
[email protected]) ABSTRACT A new lithostratigraphical framework for Singapore is proposed, based on the analysis of c. 20,000 m of core recovered from 121 c. 205 m deep boreholes and augmented with 218 field localities from across Singapore. The new framework describes a succession dating from the Carboniferous to the Quaternary. New U-Pb detrital zircon dates and fossil analysis were used to constrain the ages of key sedimentary units. The oldest known sedimentary rocks in Singapore are found to be the deformed Carboniferous (Mississippian) Sajahat Formation. These are succeeded by the newly erected, Middle and Upper Triassic, marine to continental Jurong Group and Sentosa Group successions that accumulated in the southern part of the Semantan Basin. The Jurong Group comprises four formations: the Tuas Formation, the Pulau Ayer Chawan Formation, the Pandan Formation and the Boon Lay Formation. The Sentosa Group contains two formations: the Tanjong Rimau Formation and the Fort Siloso Formation. In Singapore, the depositional record during this time is related to late Permian to Triassic arc magmatism in the southern part of the forearc basin to the Sukhothai Arc.