Structural Patterns of Thrust-Related Folds of Deepwater Fold and Thrust Belts in NW Borneo
-
摘要: 深水褶皱冲断带的构造形态和特征会随着时间而变化进而影响深水油气勘探开发，而针对这个方面的研究在西北婆罗洲褶皱冲断带内相对薄弱.利用地震和地质相结合的方法，确定了逆冲相关褶皱的构造样式，探讨了其形成演化过程和主控因素，建立了研究区逆冲相关褶皱成藏模式.结果表明：研究区深水褶皱冲断带内发育隐伏型、顶部断裂型、滑塌型以及埋藏型4种逆冲相关褶皱构造样式，且平面上这4种逆冲相关褶皱自海向陆依次发育，其中隐伏型背斜褶皱幅度较低，海底无突出地形显示，主要发育于褶皱冲断带最前端；顶部断裂型背斜在海底有清晰的地形显示，以背斜顶部断裂发育为特征；滑塌型背斜顶部受正断层效应影响，翼部发育块体滑塌沉积；埋藏型背斜主要发育于现今陆架边缘附近，上覆厚层沉积层，在海底无突出地形表现.研究区所发育的4种逆冲相关褶皱构造是成因上有密切联系的统一整体，一个典型逆冲相关褶皱的形成大致经历滑脱、初始逆冲、强烈逆冲和埋藏4个阶段，依次发育隐伏型、顶部断裂型、滑塌型以及埋藏型4种背斜构造样式.同时，沿逆冲褶皱冲断带走向，受地形、沉积物供给、天然气水合物发育等因素控制，在同一挤压应力作用下，不同部位发育的逆冲相关褶皱样式存在差异性.在这种特殊的构造背景下，研究区发育独特的断裂控藏模式，极具勘探潜力.Abstract: The structure and characteristics of deepwater fold and thrust belts (DFTBs) can change with time and thus affect the exploration and development of deepwater oil and gas, while the research on this aspect is relatively weak in the DFTBs of NW Borneo. Based on the combination method of seismic and geology, this paper determines the structural patterns of thrust-related folds, discusses the formation process and controlling factors, establishes the accumulation model of thrust-related folds in the study area. The results show that four types of structural patterns of thrust-related folds develop in the DFTBs of NW Borneo, namely, hidden type, crest faulted type, slump type and buried type, and on the planar the above four type thrust-related folds successively distribute from sea to land. The amplitude of anticline fold of hidden type is relatively low, with no obvious seafloor expression, mainly forming in the foremost of DFTBs. The crest faulted type is characterized by the development of faults in the crest of anticline, with apparent seafloor relief. The crest of slump type anticline is influenced by the normal faults, with flanks associated with slides and slumps. The buried type anticlines mainly develop close to the shelf margin, buried by a thick sedimentary overburden, with no prominent seafloor expression. Four type thrust-related folds structures stage, with hidden type, crest faulted type, slump type and buried type anticline, successively developed. At the same time, if viewed along the strike of the DFTBs, there are significant variations in the geometry of laterally corresponding thrust-related folds under the same compression, controlled by the topography, differential sediment input and the development of subsurface gas hydrates. Under this special tectonic background, a unique fault-controlled accumulation model forms in the study area, with favorable exploration potential.
-
Key words:
- deepwater fold and thrust belt /
- thrust structure /
- anticline /
- structural style /
- NW Borneo /
- South China Sea /
- petroleum geology
-
图 1 西北婆罗洲构造纲要图
Fig. 1. Schematic structural map showing key tectonic elements in NW Borneo
图 3 西北婆罗洲深水褶皱冲断带典型深度域地震剖面及解释结果
剖面位置见图 1
Fig. 3. Typical depth-migrated seismic sections and interpreted results of deepwater fold and thrust belt of NW Borneo
图 4 西北婆罗洲深水褶皱冲断带逆冲相关褶皱构造样式
剖面位置见图 3
Fig. 4. Thrust-related fold styles of deepwater fold and thrust belt in NW Borneo
图 5 西北婆罗洲深水褶皱冲断带逆冲相关褶皱分布规律
剖面位置见图 1
Fig. 5. The distribution of thrust-related fold of deepwater fold and thrust belt in NW Borneo
图 6 西北婆罗洲深水褶皱冲断带逆冲相关褶皱形成演化过程示意图
不同颜色代表了地层沉积的先后顺序
Fig. 6. Schematic illustration of evolution of thrust-related fold of deepwater fold and thrust belt in NW Borneo
图 7 西北婆罗洲深水褶皱冲断带逆冲相关褶皱形成主控因素
a.海底地形；b.文莱近海和沙巴深水区上新世—全新世地层等厚图，据Morley and Back(2008)修改；c.研究区天然气水合物分布
Fig. 7. Controlling factors of thrust-related fold of deepwater fold and thrust belt in NW Borneo
-
[1] Briais, A., Patriat, P., Tapponnier, P., 1993.Updated Interpretation of Magnetic Anomalies and Seafloor Spreading Stages in the South China Sea:Implications for the Tertiary Tectonics of Southeast Asia.Journal of Geophysical Research:Solid Earth, 98(B4):6299-6328. https://doi.org/10.1029/92jb02280 [2] Bugge, T., 1983.Submarine Slides on the Norwegian Continental Margin, with Special Emphasis on the Storegga Area (Dissertation).Continental Shelf Institute, Trondheim, 110-152. [3] Cullen, A.B., 2010.Transverse Segmentation of the Baram-Balabac Basin, NW Borneo:Refining the Model of Borneo's Tectonic Evolution.Petroleum Geoscience, 16(1):3-29. https://doi.org/10.1144/1354-079309-828 [4] Deng, R.J., Deng, Y.H., Yu, S., et al., 2008.Hydrocarbon Geology and Reservoir Formation Characteristics of Niger Delta Basin.Petroleum Exploration and Development, 35(6):755-762(in Chinese with English abstract). [5] Field, M.E., 1990.Submarine Landslides Associated with Shallow Seafloor Gas and Gas Hydrates off Northern California.AAPG Bulletin, 74:971-972. https://doi.org/10.1306/44b4c3e6-170a-11d7-8645000102c1865d [6] Franke, D., Barckhausen, U., Heyde, I., et al., 2008.Seismic Images of a Collision Zone Offshore NW Sabah/Borneo.Marine and Petroleum Geology, 25(7):606-624. https://doi.org/10.1016/j.marpetgeo.2007.11.004 [7] Gong, G.C., Liu, K.K., Liu, C.T., et al., 1992.The Chemical Hydrography of the South China Sea West of Luzon and a Comparison with the West Philippine Sea.Terrestrial, Atmospheric and Oceanic Sciences, 3(4):587-602. https://doi.org/10.3319/tao.1992.3.4.587(o) [8] Hall, R., 1996.Reconstructing Cenozoic SE Asia.Geological Society, London, Special Publication, 106:153-184. https://doi.org/10.1144/gsl.sp.1996.106.01.11 [9] Hall, R., Wilson, M.E.J., 2000.Neogene Sutures in Eastern Indonesia.Journal of Asian Earth Sciences, 18(6):781-808. https://doi.org/10.1016/s1367-9120(00)00040-7 [10] Hall, R., van Hattum, M.W.A., Spakman, W., 2008.Impact of India-Asia Collision on SE Asia:The Record in Borneo.Tectonophysics, 451:366-389. https://doi.org/10.1016/j.tecto.2007.11.058 [11] Han, B., Zhu, B.D., Wan, L., et al., 2015.Deep-Water Fold and Thrust Tectonics in Southeastern Nansha Trough.Geological Review, 61(5):1061-1067(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP201505009.htm [12] Hazebroek, H.P., Tan, D.N.K., 1993.Tertiary Tectonic Evolution of the NW Sabah Continental Margin.Bulletin of the Geological Society of Malaysia, 33:195-210. https://doi.org/10.1306/f4c8fb24-1712-11d7-8645000102c1865d [13] He, D.F., Jia, C.Z., 2005.Thrust Tectonics and Hydrocarbon Accumulation.Petroleum Exploration and Development, 32(2):55-62(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-skyk20050200d.htm [14] Hesse, S., Back, S., Franke, D., 2009.The Deep-Water Fold-and-Thrust Belt Offshore NW Borneo:Gravity-Driven versus Basement-Driven Shortening.Geological Society of America Bulletin, 121(5-6):939-953. https://doi.org/10.1130/b26411.1 [15] Hesse, S., Back, S., Franke, D., 2010a.The Structural Evolution of Folds in a Deepwater Fold and Thrust Belt-A Case Study from the Sabah Continental Margin Offshore NW Borneo, SE Asia.Marine and Petroleum Geology, 27(2):442-454. https://doi.org/10.1016/j.marpetgeo.2009.09.004 [16] Hesse, S., Back, S., Franke, D., 2010b.Deepwater Folding and Thrusting Offshore NW Borneo, SE Asia.Geological Society, London, Special Publications, 348(1):169-185. https://doi.org/10.1144/sp348.9 [17] Hinz, K., Fritsch, J., Kempter, E.H.K., et al., 1989.Thrust Tectonics along the North-Western Continental Margin of Sabah/Borneo.Geologische Rundschau, 78(3):705-730. https://doi.org/10.1007/bf01829317 [18] Hovland, M., Gudmestad, O.T., 2013.Potential Influence of Gas Hydrates on Seabed Installations.Geophysical Monograph Series, 124:307-315. https://doi.org/10.1029/gm124p0307 [19] Hutchison, C.S., 1996a.The "Rajang Accretionary Prism" and "Lupar Line" Problem of Borneo.Geological Society, London, Special Publication, 106(1):247-261. https://doi.org/10.1144/gsl.sp.106.01.16 [20] Hutchison, C.S., 1996b.South-East Asian Oil, Gas, Coal and Mineral Deposits.In:Menzies, M.A., ed., Oxford Monographs on Geology and Geophysics.Clarendon Press, Oxford. [21] Hutchison, C.S., Bergman, S.C., Swauger, D.A., et al., 2000.A Miocene Collisional Belt in North Borneo:Uplift Mechanism and Isostatic Adjustment Quantifıed by Thermochronology.Journal of the Geological Society, 157:783-793. https://doi.org/10.1144/jgs.157.4.783 [22] Ingram, G.M., Chisholm, T.J., Grant, C.J., et al., 2004.Deepwater North West Borneo:Hydrocarbon Accumulation in an Active Fold and Thrust Belt.Marine and Petroleum Geology, 21(7):879-887. https://doi.org/10.1016/j.marpetgeo.2003.12.007 [23] James, D.M.D., 1984.The Geology and Hydrocarbon Resources of Negara Brunei Darussalam.Brunei Museum and Brunei Shell Petroleum Company, Syabas Bandar Seri Begawan. [24] Kayen, R.E., Lee, H.J., 1990.Seafloor Landslides in Regions of Gas Hydrate, a Global Change Perspective.AAPG Bulletin, 74:982-983. https://doi.org/10.1306/20b22125-170d-11d7-8645000102c1865d [25] Lambiase, J.J., Cullen, A.B., 2013.Sediment Supply Systems of the Champion "Delta" of NW Borneo:Implications for Deepwater Reservoir Sandstones.Journal of Asian Earth Sciences, 76:356-371. https://doi.org/10.1016/j.jseaes.2012.12.004 [26] Lei, C., Ren, J.Y., Zhang, J., 2015.Tectonic Province Divisions in the South China Sea:Implication for Basin Geodynamics.Earth Science, 40(4):744-762(in Chinese with English abstract). https://doi.org/10.3799/dqkx.2015.062 [27] Levell, B.K., 1987.The Nature and Signifıcance of Regional Unconformities in the Hydrocarbon-Bearing Neogene Sequence Offshore West Sabah.Geological Society of Malaysia Bulletin, 21:55-90. http://www.gsm.org.my/content.php?id=54&pid=702001-101135 [28] Li, S.Q., Tang, P.C., Rao, G., 2013.Cenozoic Deformation Characteristics and Controlling Factors of Kalayuergun Structural Belt, Kuqa Fold and Thrust Belt, Southern Tianshan.Earth Science, 38(4):859-869(in Chinese with English abstract). https://doi.org/10.3799/dqkx.2013.084 [29] Lynn, H.B., Deregowski, S., 1981.Dip Limitations on Migrated Sections as a Function of Line Length and Recording Time.Geophysics, 46(10):1392-1397. https://doi.org/10.1190/1.1441146 [30] MacLeod, M.K., 1982.Gas Hydrates in Ocean Bottom Sediments.AAPG Bulletin, 66(12):2649-2662. https://doi.org/10.1306/03b5ac8c-16d1-11d7-8645000102c1865d [31] Milsom, J., Holt, R., Ayub, D.B., et al., 1997.Gravity Anomalies and Deep Structural Controls at the Sabah-Palawan Margin, South China Sea.In:Frazer, A.J., Matthews, S.J., Murphy, R.W., eds., Petroleum Geology of Southeast Asia.Geological Society, London, Special Publication, 126:417-427.https://doi.org/10.1144/gsl.sp.1997.126.01.25 [32] Morley, C.K., 2007a.Interaction between Critical Wedge Geometry and Sediment Supply in a Deep-Water Fold Belt.Geology, 35(2):139. https://doi.org/10.1130/g22921a.1 [33] Morley, C.K., 2007b.Development of Crestal Normal Faults Associated with Deepwater Fold Growth.Journal of Structural Geology, 29(7):1148-1163. https://doi.org/10.1016/j.jsg.2007.03.016 [34] Morley, C.K., 2009.Growth of Folds in a Deep-Water Setting.Geosphere, 5(2):59-89. https://doi.org/10.1130/ges00186.1 [35] Morley, C.K., Back, S., 2008.Estimating Hinterland Exhumation from Late Orogenic Basin Volume, NW Borneo.Journal of the Geological Society, 165(1):353-366. https://doi.org/10.1144/0016-76492007-067 [36] Morley, C.K., Back, S., van Rensbergen, P., et al., 2003.Characteristics of Repeated, Detached, Miocene-Pliocene Tectonic Inversion Events, in a Large Delta Province on an Active Margin, Brunei Darussalam, Borneo.Journal of Structural Geology, 25(7):1147-1169. https://doi.org/10.1016/s0191-8141(02)00130-x [37] Morley, C.K., King, R., Hillis, R., et al., 2011.Deepwater Fold and Thrust Belt Classification, Tectonics, Structure and Hydrocarbon Prospectivity:A Review.Earth-Science Reviews, 104(1-3):41-91. https://doi.org/10.1016/j.earscirev.2010.09.010 [38] Ou, C.H., Chen, W., Han, Y.Z., et al., 2016.Geometric Analysis and Kinematic Simulation of Oblique-Thrust Fault-Related-Fold of Buzurgan Anticline in Zagros Basin.Earth Science, 41(3):385-393(in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.030 [39] Petronas, 1999.The Petroleum Geology and Resources of Malaysia.Petoliam Nasional Berhad, Kuala Lumpur. [40] Rowan, M.G., Peel, F.J., Vendeville, B.C., 2004.Gravity-Driven Fold Belts on Passive Margins.In:McClay, K.R., ed., Thrust Tectonics and Hydrocarbon Systems.American Association of Petroleum Geologists, Tulsa. [41] Sandal, S.T., 1996.The Geology and Hydrocarbon Resources of Negara Brunei Darussalam.Brunei Shell Petroleum Company/Brunei Museum, Syabas Bandar Seri Begawan. [42] Sarnthein, M., Pflaumann, U., Wang, P.X., et al., 1994.Preliminary Report on Sonne-95 Cruise "Monitor Monson" to the South China Sea.Geologisch-Palaontologisches Institut und Museum, Christian-Albrechts-Universitat, Kiel. [43] Sloan, E.D., Koh, C.A., 1990.Clatherate Hydrates of Natural Gases.CRC Press, Boca Raton. [44] Strayer, L.M., Erickson, S.G., Suppe, J., 2004.Influence of Growth Strata on The Evolution of Fault-Related Folds-Distinct-Element-Models.In:McClay, K.R.ed., Thrust Tectonics and Hydrocarbon Systems.American Association of Petroleum Geologists, Tulsa. [45] Taylor, B., Hayes, D.E., 1983.Origin and History of the South China Sea Basin.In:Hayes, D.E., ed., The Tectonic and Geologic Evolution of Southeastern Asian Seas and Islands:Part 2.American Geophysical Union, Washington D.C.. [46] van Hattum, M.W.A., Hall, R., Pickard, A.L., et al., 2006.Southeast Asian Sediments not from Asia:Provenance and Geochronology of North Borneo Sandstones.Geology, 34(7):589-592. https://doi.org/10.1130/g21939.1 [47] 邓荣敬, 邓运华, 于水, 等, 2008.尼日尔三角洲盆地油气地质与成藏特征.石油勘探与开发, 35(6):755-762. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=skyk200806022&dbname=CJFD&dbcode=CJFQ [48] 韩冰, 朱本铎, 万玲, 等, 2015.南沙海槽东南缘深水逆冲推覆构造.地质论评, 61(5):1061-1067. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzlp201505009&dbname=CJFD&dbcode=CJFQ [49] 何登发, 贾承造, 2005.冲断构造与油气聚集.石油勘探与开发, 32(2):55-62. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=skyk20050200d&dbname=CJFD&dbcode=CJFQ [50] 雷超, 任建业, 张静, 2015.南海构造变形分区及成盆过程.地球科学, 40(4):744-762. https://doi.org/10.3799/dqkx.2015.062 [51] 李世琴, 唐鹏程, 饶刚, 2013.南天山库车褶皱-冲断带喀拉玉尔滚构造带新生代变形特征及其控制因素.地球科学, 38(4):859-869. https://doi.org/10.3799/dqkx.2013.084 [52] 欧成华, 陈伟, 韩耀祖, 等, 2016.扎格罗斯盆地Buzurgan背斜斜向逆冲断裂褶皱的几何解析及运动学模拟.地球科学, 41(3):385-393. https://doi.org/10.3799/dqkx.2016.030 -
下载:
点击查看大图
图(8)
计量
- 文章访问数: 3100
- HTML全文浏览量: 1075
- PDF下载量: 20
- 被引次数: 0
