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Starting of final convergence between the Palawan Continental Terrane and northern Borneo‐SW Philippines (∼21 Ma) likely caused regional uplift/thrusting, forming the Top Crocker Unconformity and triggering the NW‐dipping Celebes Sea subduction. One well even had oil and gas shows in MDT samples. Objects, Solid Surface A garment similar to a sarong, worn by Melanesians, as in the Fiji Islands. The Cenozoic Sulu Sea arc‐basin system is situated in the tectonic junction between the South China Sea (SCS), northern Borneo, Palawan Continental Terrane, Philippine Mobile Belt, and Celebes Sea. NW‐dipping Celebes Sea subduction largely ceased after ∼9 Ma, followed by extension‐related uplift/exhumation and 4–0.2 Ma intraplate volcanism in northern Borneo. km. lb). Geophysics, Biological 6). Holes were drilled at three Sites in the Sulu Sea on Ocean Drilling Program Leg 124. Processes, Information The Middle Eocene (42.65 Ma) Sabah ophiolite and Eocene‐Oligocene (34–33 Ma) Central Palawan ophiolite have MORB‐IAT‐transitional features, representing an intra‐oceanic subduction setting in the Paleogene northern Borneo and central‐southern Palawan. It is 650 km long and 400 km wide, located between the South China Sea to the north and the Celebes Sea to the south (Fig. across the deep basin of Sulu–Celebes Sea could introduce. The final edited and typeset version of record will appear in the future. Geology and Geophysics, Physical Sulawesi Sea is linked with the Sulu Sea through a … The Sulu Sea basin extends to the northeast portion of Sabah where there have been gas discoveries. By continuing to use our website, you are agreeing to our, Cushman Foundation for Foraminiferal Research, Mineralogical Society of Great Britain and Ireland. Planets, Magnetospheric more accurate for those satellite-detected IWs adjacent to. The papers presented at those meetings are contained in this volume. Unlimited viewing of the article/chapter PDF and any associated supplements and figures. Search for other works by this author on: You do not currently have access to this chapter. Properties of Rocks, Computational Oceanography, Interplanetary Physics, Solar 1). The Sandakan Sub-basin, located in the southern Sulu Sea Basin (Figure 1), is different from other parts of the region and different from most basins within the Philippines. Afterward, to the west of the Sulu Sea, within‐plate extension in northern Borneo occurred and continues to the present‐day; whereas to the east, subduction of the Sulu Sea may have occurred along the Negros‐Sulu trenches, and produced arc volcanism from ∼4 Ma. The Sulu Trench marks the boundary of the Sulu micro-block with the Sulu Sea basin and the Palawan micro-block. What does sulu mean? All-Filipino firm Sulu Sea Energy Resources Development Corp. (SSERDC) is eyeing a contract for an offshore area within the Sulu Sea basin (PDA No. The 260,000 sq. 1993). Physics, Astrophysics and Astronomy, Perspectives of Earth and Space Scientists, orcid.org/https://orcid.org/0000-0003-2245-4014, orcid.org/https://orcid.org/0000-0002-3203-039X, orcid.org/https://orcid.org/0000-0003-2741-6076, orcid.org/https://orcid.org/0000-0003-1949-8673, orcid.org/https://orcid.org/0000-0001-7440-732X, orcid.org/https://orcid.org/0000-0003-4083-4811, I have read and accept the Wiley Online Library Terms and Conditions of Use. Knowledge of continental margins advanced rapidly during the 1970s. Geophysics, Mathematical We compare new/published geochronological and geochemical data from across the circum‐Sulu Sea region, and summarize seven major magmatic phases from the Middle Eocene to Pleistocene. Sulu Sea Province (Miocene TPS) Sandakan Reservoirs AU 1.0 Oil 178 58 231 997 339 84 345 1,536 515 3 11 53 18 Gas 2,448 2,211 6,907 18,205 8,159 26 84 234 101 Baram Delta/Brunei-Sabah Basin Province (Brunei-Sabah TPS) Brunei-Sabah Deltaics AU 1.0 Oil 67 350 608 1,012 635 1,208 2,165 3,678 2,269 23 41 70 43 "The Sulu Sea: A Marginal Basin in Southeast Asia", Geological and Geophysical Investigations of Continental Margins, Joel S. Watkins, Lucien Montadert, Patricia Wood Dickerson. The Sandakan basin lies in the southwestern Sulu Sea straddling the Philippines/Malaysia maritime border (Fig. establishing a regional geologic framework The data coverage and quality are appropriate for. The area of each basin ranges from 36,000 sq km to 92,000 sq km (Sulu Sea is bigger but it is partly covered by oceanic crust). errors [50]. According to the magnetics model, it is likely that the Sulu Sea Basin started to open at 30-35 Ma (early Oligocene) with 0.6 cm/yr half-spreading rate. Please check your email address / username and password and try again. Spreading continued until at least 10 Ma (early upper Miocene). When and how these sea basins were created are long disputed. Most of the oceanic crust is already subducted. The Sulu Sea basin may have continued to expand till ∼9 Ma, when NW‐dipping subduction of the Celebes Sea stopped. The Sulu Sea basin consists of the Sandakan sub-basin while the East Palawan basin is divided into the Balabac and Bancauan sub-basins. Sulawesi Sea is a semi-enclosed basin, surrounded by Philippines, Sulu Archipelago, Kalimantan Island, North Sulawesi and Sangihe Islands. American Association of Petroleum Geologists, © American Association of Petroleum Geologists 1979, ISBN 978-1-62981-193-2$24.00, This site uses cookies. A. Mascle, P. A. Biscarrat, 1979. Learn about our remote access options, Faculty of Science, Universiti Brunei Darussalam, Gadong, BE1410 Brunei Darussalam, State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China, SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey, TW20 0EX UK, Centre for Ore Deposit and Earth Sciences (CODES), University of Tasmania, Tasmania, 7001 Australia, National Institute of Geological Sciences, University of the Philippines Diliman, Philippines, Department of Geological Engineering, Universitas Gadjah Mada, Yogyakarta, Indonesia, This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process, which may lead to differences between this version and the Version of Record. To better disseminate new knowledge of continental margins, AAPG held three meetings in 1977 to review the current status of knowledge. RESEARCH PROJECTS BROWSE BY LOCATION Sulu Sea Basin Projects. Please check your email for instructions on resetting your password. If you do not receive an email within 10 minutes, your email address may not be registered, Log in with your society credentials Our model suggests that the Sulu Sea was formed by the NW‐dipping Celebes Sea subduction at ∼21 Ma, in response to the collision between the South China‐derived Palawan Continental Terrane and northern Borneo‐SW Philippines. The Southeast Sulu Sea is a small oceanic basin that opened in Middle Miocene time in a back-arc setting along the Sundaland margin during subduction of the Celebes Sea plate beneath the Sulu arc. Data incorporated in this analysis includes 2D seismic, gamma-ray logs, biostratigraphy and cuttings You could not be signed in. The opening and closure (when Australia‐Eurasia eventually collide) of these basins represent the final tectonic episode of the Neo‐Tethys, an ocean that separates the northern and southern continents. AbstractThe Cenozoic Sulu Sea arc‐basin system is situated in the tectonic junction between the South China Sea (SCS), northern Borneo, Palawan Continental Terrane, Philippine Mobile Belt, … The basin has high potential but is under-explored. (noun) Thus, the estimated generation time for IWs are. and Petrology, Exploration The 40,000 sq km basin contains as much as 8,000 m of Neogene deltaic May 10th, 1993 The basin extends to the north-east portion of Sabah in Borneo where there have been gas discoveries, another indication of … “These petroleum reserves calculations are based on the 16 sedimentary basins situated all over the country from the Cagayan Valley Basin in the north down to the Agusan-Davao Basin in the south as well as the prolific Northwest Palawan Basin and the Sulu Sea Basin along the western flank of the archipelago,” the DOE said. Learn more. Geophysics, Geomagnetism and Chemical Oceanography, Physical and Paleomagnetism, History of All-Filipino firm Sulu Sea Energy Resources Development Corp. (SSERDC) is eyeing a contract for an offshore area within the Sulu Sea basin … in Modeling Earth Systems (JAMES), Journal of Geophysical Research From the Middle Eocene to Early Miocene the Sandakan Sub-basin was affected by the opening of the South China Sea. The Sulu Sea Basin, by contrast, is a delta superimposed on a back-arc basin where expected play types are carbonate reef build-ups, anticlines and fault blocks. Introduction Figure 1:Configuration and bathymetry of the Sulawesi Sea (m). Processes in Geophysics, Atmospheric After the SCS opening (∼32 Ma) and ridge jump (∼25 Ma), late‐stage Proto‐SCS subduction (24–21 Ma) may have formed the Panay arc andesite and the BABB magmatism in SW Zamboanga peninsula. The Sulu Sea region is composed of the East Palawan and the Sulu Sea basins including the sub-basins of Balabac, Bancauan and Sandakan. If you have previously obtained access with your personal account, please log in. 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