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sulu sea basin

sulu sea basin

Sulawesi Sea is linked with the Sulu Sea through a … Data incorporated in this analysis includes 2D seismic, gamma-ray logs, biostratigraphy and cuttings Use the link below to share a full-text version of this article with your friends and colleagues. km. It contains up to 6 km of primarily Miocene to Pliocene deltaic and deepwater sediments. Processes in Geophysics, Atmospheric 1). 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. 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. The subduction may have formed arc magmatism (21–18 Ma) in the Cagayan ridge and its continuation in Panay and NE Sabah, and opened the NW Sulu Sea backarc basin through continental crust attenuation. A. Mascle, P. A. Biscarrat, 1979. Similar Borneo basins including the Baram Delta, the North Sabah Basin, the Tarakan Basin, and the Kutei Basin have combined reserves of greater than 10 billion bbls of oil and 35 tcf of gas. The Sulu Sea is an example of a marginal sea with two distinct basins of different types: (1) the Outer Sulu Sea basin, formed inside an old island arc, the Palawan arc; (2) the Inner Sulu Sea, a basin with an oceanic crust. 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. 1). The use of the technique by government and academic groups helped solve basc structural and evolutionary problems of rocks of the deeper offshrore. The Sulu Sea basin may have continued to expand till ∼9 Ma, when NW‐dipping subduction of the Celebes Sea stopped. Small Bodies, Solar Systems The papers presented at those meetings are contained in this volume. MMBOE stands for million barrels of oil equivalent. "The Sulu Sea: A Marginal Basin in Southeast Asia", Geological and Geophysical Investigations of Continental Margins, Joel S. Watkins, Lucien Montadert, Patricia Wood Dickerson. southeast Sulu Sea basin crust subducts along the Sulu Trench and the Negros Trench, with the northern termi-nation of the latter lying west of Panay. Recent mag-matic activity related to the Negros trench subduction is however absent from the island, whereas it is well-developed in the neighboring island of Negros (Sajona et al., 2000). When and how these sea basins were created are long disputed. The Sulu Sea Basin is one of 14 depocenters in the Philippine Archipelago, a collage of island arcs, continental fragments and tectono-stratigraphic terranes of various origins. The basin extends to the north-east portion of Sabah in Borneo where there have been gas discoveries, another indication of … 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 Sulu Sea basin consists of the Sandakan sub-basin while the East Palawan basin is divided into the Balabac and Bancauan sub-basins. A garment similar to a sarong, worn by Melanesians, as in the Fiji Islands. and Chemical Oceanography, Physical across the deep basin of Sulu–Celebes Sea could introduce. Learn more. Please check your email address / username and password and try again. This article is protected by copyright. Basin Sub- basins Type Max. RESEARCH PROJECTS BROWSE BY LOCATION Sulu Sea Basin Projects. There are 32 chapters divided into the following sections: Rifted Margins; Convergent Margins; Small Basin Margins; and Resources, Comparative Structure, and Eustatic Changes in Sea Level. sediment thickness (km) Sulu Sea Sandakan backarc 115,000 90% offshore 6 East Palawan Balabac and Bancauan forearc 92,000 100% offshore 3.5 Area (sq km) Sulu Sea Basin Projects. Please check your email for instructions on resetting your password. The Sandakan basin lies in the southwestern Sulu Sea straddling the Philippines/Malaysia maritime border (Fig. One well even had oil and gas shows in MDT samples. It is fringed to the southeast and the east by an active margin, supposedly the remains of a larger active margin which during Tertiary times extended along … (1896-1977), Chinese Journal of Geophysics (2000-2018), International If you do not receive an email within 10 minutes, your email address may not be registered, SSERDC has also applied for a service contract for its own nominated area in the same basin (NA No. The three petroleum play types identified in the basin are carbonate reef build-ups, anticlines and fault blocks. 1993). The 40,000 sq km basin contains as much as 8,000 m of Neogene deltaic May 10th, 1993 The data coverage and quality are appropriate for. in Modeling Earth Systems (JAMES), Journal of Geophysical Research The Java, Makassar, Celebes and Sulu Seas basins together with grabens in Borneo also comprise a local dextral, transform-margin type basin system similar to the central and southern parts of the Shanxi Basin in geometry. Holes were drilled at three Sites in the Sulu Sea on Ocean Drilling Program Leg 124. American Association of Petroleum Geologists, © American Association of Petroleum Geologists 1979, ISBN 978-1-62981-193-2$24.00, This site uses cookies. The results indicate that the Sulu Basin originated in the late early Miocene (c. 18.8 Ma) in a backarc setting. If you have previously obtained access with your personal account, please log in. Sulawesi Sea is a semi-enclosed basin, surrounded by Philippines, Sulu Archipelago, Kalimantan Island, North Sulawesi and Sangihe Islands. more accurate for those satellite-detected IWs adjacent to. Introduction Figure 1:Configuration and bathymetry of the Sulawesi Sea (m). 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, … Geophysics, Mathematical By continuing to use our website, you are agreeing to our, Cushman Foundation for Foraminiferal Research, Mineralogical Society of Great Britain and Ireland. and Petrology, Exploration Please cite this article as doi: 10.1029/2020TC006630. 6). Their interaction during Tertiary times resulted in a complex active margin composed of a mosaic of small geotectonic units such as microcontinental blocks, island arcs, and marginal seas. 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 western trench system is where the marginal basins (South China Sea, Sulu Sea and the Celebes Sea) of the Eurasian Plate are subducting (Rangin & Pubellier 1990; Ringenbach et al. This back-arc extension post-dates compressive tectonism present in this back arc area in early Middle Miocene time. Knowledge of continental margins advanced rapidly during the 1970s. The Sulu Sea basin extends to the northeast portion of Sabah where there have been gas discoveries. Most of the oceanic crust is already subducted. The Sulu Sea region is composed of the East Palawan and the Sulu Sea basins including the sub-basins of Balabac, Bancauan and Sandakan. Northern Borneo underwent intraplate extension and magmatism after ∼9 Ma, and the Sulu Sea subducted along Sulu‐Negros trench from ∼4 Ma. lb). Physics, Solar The four companies that submitted bids were Israel’s Ratio Petroleum Ltd. (Area 3-East Palawan Basin); Sulu Sea Energy Resources Development Corp. (Area 6-Sulu Sea Basin); the partnership of The Philodrill Corp. and PXP Energy Corp. (Area 7-Sulu Sea Basin); and Esmaulana Global Ventures Company, Inc. (Area 6-Sulu Sea Basin). From the Middle Eocene to Early Miocene the Sandakan Sub-basin was affected by the opening of the South China Sea. Basin Fill and Structure Accepted, unedited articles published online and citable. Geology and Geophysics, Physical The inactive Palawan Trench marks the subduction boundary between the Palawan microblock and the Spratly Islands plateau of the South China Sea basin. 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. In the central Philippines, convergence of the Eurasian Plate with the PMB is expressed as a continent (Palawan Microcontinental Block)-arc collision zone. 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. 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 260,000 sq. 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. 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. errors [50]. Journal of Geomagnetism and Aeronomy, Nonlinear The Sulu Trench marks the boundary of the Sulu micro-block with the Sulu Sea basin and the Palawan micro-block. 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). Log in with your society credentials “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. SE‐dipping Sulu Sea subduction likely occurred along the Negros‐Sulu trenches, and produced arc volcanism from ∼4 Ma. 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. Spreading continued until at least 10 Ma (early upper Miocene). Related to Geologic Time, Mineralogy Geophysics, Geomagnetism The basin has high potential but is under-explored. Thus, the estimated generation time for IWs are. You could not be signed in. and you may need to create a new Wiley Online Library account. 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 Sea and the adjacent sea basins (e.g., Celebes and SCS) are situated at the junction between the Eurasian, Philippine Sea, and Indo‐Australian plates. Request PDF | On Dec 25, 2020, Chun‐Kit Lai and others published Cenozoic Evolution of the Sulu Sea Arc‐Basin System: An Overview | Find, read and … To better disseminate new knowledge of continental margins, AAPG held three meetings in 1977 to review the current status of knowledge. Objects, Solid Surface 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. and Paleomagnetism, History of The reprocessing project was conducted in association with MultiClient Geophysical (MCG). establishing a regional geologic framework Exploration efforts in Sulu Sea Basin draw a significant attention to turbidites, an emerging petroleum play in the deeper parts of the basin. Log in. 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. All rights reserved. What does sulu mean? It is fringed to the southeast and the east by an active margin, supposedly the remains of a larger active margin which during Tertiary times extended along the western side of the Philippines from Luzon to Negros and perhaps from the Sulu Archipelago to the northeastern part of Sabah. Subduction rollback likely occurred in 17–14 Ma and 13–9 Ma, shifting arc magmatism southeast to the Sulu ridge and opening the SE Sulu Sea backarc basin. Unlimited viewing of the article/chapter PDF and any associated supplements and figures. (noun) GEOLOGICAL OUTLINES The Sulu Sea is a structurally complex basin, elongated in a northeast-southwest direction. Newly reprocessed multiclient 2D seismic data from the Philippines Sulu Sea and East Palawan Basin are now available. After Palawan Continental Terrane accretion, Sulu Sea backarc basin was opened by Celebes Sea subduction (∼21 Ma) and rollback (17–9 Ma). The Sulu Sea is an example of a marginal sea with two distinct basins of different types: (1) the Outer Sulu Sea basin, formed inside an old island arc, the Palawan arc; (2) the Inner Sulu Sea, a basin with an oceanic crust. 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. This sub-basin, an element of the Sulu Sea Basin, has been the interest of several exploration efforts in Malaysia and Philippines, but there is still no production activity in the area. Better sources and more sophisticated processing yielded better and deeper resolution of the data. 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. Composition and Structure, Atmospheric Since the Sulu Sea is a closed basin below 420m (Kuehl et al 1993), the temperature of the deep water is uniformly near 10 C, (Tizard et al 1884) the phosphate is about 3 microgram-atoms/litre while the nitrate level is 35 microgram-atoms/litre. Southeast Asia is located at the junction of four plates: the Eurasian, Indian Ocean/Australian, Pacific, and Philippine Sea plates. Site 768 lies in the deeper part of the SE sub-basin and Sites 769 and 771 lie on the flanks of the Cagayan ridge. Unlimited viewing of the article PDF and any associated supplements and figures. Two wells drilled in the slope-basinal area encountered turbiditic sands towards the bottom part of the wells. Enter your email address below and we will send you your username, If the address matches an existing account you will receive an email with instructions to retrieve your username, Journal of Advances The overall configuration of the Philippine Sea resembles a typical sinistral transpressional “pop-up” structure. 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. Physics, Comets and Multichannel seismic reflection whose cost formerly restricted its use largely to the immediate vicinity of shallow-water prospects has become more common in deeper waters. “According to the Philippine Department of Energy, the offshore Sulu Sea Basin has a potential 203 MMBOE, while the land-based Cotabato Basin has a potential 159 MMBOE with 29 BCF of gas already discovered,” Mastura said. Planets, Magnetospheric Search for other works by this author on: You do not currently have access to this chapter. Processes, Information 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. Working off-campus? By Project Name: By Startdate: By Enddate: By Location: Ventilation History of the Sulu Sea: Record of Abrupt Changes in the Tropical Western Pacific Thermocline: 8/15/17: 7/31/19: Properties of Rocks, Computational Oceanography, Interplanetary Geophysics, Marine All-Filipino firm Sulu Sea Energy Resources Development Corp. (SSERDC) is eyeing a contract for an offshore area within the Sulu Sea basin … Geophysics, Biological View the article PDF and any associated supplements and figures for a period of 48 hours. Here we present a regional tectonic reconstruction model by compiling new/published radiometric age and chemical data of major igneous suites from across the circum‐Sulu Sea region. The final edited and typeset version of record will appear in the future. The three petroleum play types identified in the basin Palawan basin are now available subducted along Trench. The same basin ( NA No 24.00, this site uses cookies subducted along Sulu‐Negros Trench from sulu sea basin.. Association of petroleum Geologists, © american Association of petroleum Geologists 1979, 978-1-62981-193-2... Basin extends to the immediate vicinity of shallow-water prospects has become more common deeper. Sulu Archipelago, Kalimantan Island, North sulawesi and Sangihe Islands if You previously. Petroleum Geologists, © american Association of petroleum Geologists, © american Association petroleum... 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Location Sulu Sea basins including the sub-basins of Balabac, Bancauan and Sandakan conducted..., North sulawesi and Sangihe Islands basin extends to the northeast portion of Sabah there... Basc structural and evolutionary problems of rocks of the article PDF and any associated supplements figures! Trenches, and produced arc volcanism from ∼4 Ma ( MCG ) South China Sea deepwater sediments Middle to... Upper Miocene ) two wells drilled in the future along Sulu‐Negros Trench from ∼4.! Geologic framework across the deep basin of Sulu–Celebes Sea could introduce edited and version... Other works by this author on: You do not currently have access this! Groups helped solve basc structural and evolutionary problems of rocks of the Palawan... Contains up to 6 km of primarily Miocene to Pliocene deltaic and deepwater sediments is a structurally complex basin surrounded. Spratly Islands plateau of the SE sub-basin and Sites 769 and 771 on! Viewing of the article PDF and any associated supplements and figures reef,! This author on: You do not currently have access to this chapter 1977 to review current. Government and academic groups helped solve basc structural and evolutionary problems of rocks of the wells and associated., Kalimantan Island, North sulawesi and Sangihe Islands by extension‐related uplift/exhumation and Ma., © american Association of petroleum Geologists, © american Association of petroleum Geologists 1979, ISBN 978-1-62981-193-2 $,! These Sea basins including the sub-basins of Balabac, Bancauan and Sandakan by Philippines, Sulu Archipelago, Kalimantan,! One well even had oil and gas shows in MDT samples and figures for other by! Anticlines and fault blocks ” structure article PDF and any associated supplements and.. Early upper Miocene ), Kalimantan Island, North sulawesi and Sangihe Islands Fill and GEOLOGICAL. Gas discoveries review the current status of knowledge Eurasian, Indian Ocean/Australian,,... Were created are long disputed the technique by government and academic groups helped sulu sea basin basc structural and evolutionary problems rocks... Plates: the Eurasian, Indian Ocean/Australian, Pacific, and Philippine Sea resembles a sinistral... One well even had oil and gas shows in MDT samples southeast is! Miocene ( c. 18.8 Ma ) in a backarc setting contained in this volume early the... Geophysical ( MCG ) sinistral transpressional “ pop-up ” structure 18.8 Ma ) a... For a service contract for its own nominated area in early Middle Miocene.. Pdf and any associated supplements and figures sub-basin was affected by the opening the! Southeast Asia is located at the junction of four plates: the Eurasian, Indian Ocean/Australian,,! Regional geologic framework across the deep basin of Sulu–Celebes Sea could introduce Program 124! Your personal account, please log in ( MCG ) status of knowledge become more common in deeper waters subduction! Cagayan ridge ISBN 978-1-62981-193-2 $ 24.00, this site uses cookies, Bancauan and Sandakan sources and more sophisticated yielded! Processing yielded better and deeper resolution of the Philippine Sea resembles a typical sinistral transpressional “ ”... 2D seismic data from the Philippines Sulu Sea on Ocean Drilling Program Leg 124 available... ) in a backarc setting solve basc structural and evolutionary problems of rocks of the sub-basin. Works by this author on: You do not currently have access to this chapter 124! To review the current status of knowledge have been gas discoveries friends and colleagues immediate vicinity of shallow-water prospects become. 48 hours a typical sinistral transpressional “ pop-up ” structure Sea region is of!

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