西北婆罗洲深水褶皱冲断带相关褶皱构造样式

唐武; 赵志刚; 谢晓军; 刘世翔; 王一博; 宋双; 王龙; 郭佳; 孙瑞

doi:10.3799/dqkx.2018.024

Volume 43 Issue 2

Feb. 2018

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2018 > 43(2): 491-501

Tang Wu, Zhao Zhigang, Xie Xiaojun, Liu Shixiang, Wang Yibo, Song Shuang, Wang Long, Guo Jia, Sun Rui, 2018. Structural Patterns of Thrust-Related Folds of Deepwater Fold and Thrust Belts in NW Borneo. Earth Science, 43(2): 491-501. doi: 10.3799/dqkx.2018.024

Citation:

Tang Wu, Zhao Zhigang, Xie Xiaojun, Liu Shixiang, Wang Yibo, Song Shuang, Wang Long, Guo Jia, Sun Rui, 2018. Structural Patterns of Thrust-Related Folds of Deepwater Fold and Thrust Belts in NW Borneo. Earth Science, 43(2): 491-501. doi: 10.3799/dqkx.2018.024

Citation:

Tang Wu, Zhao Zhigang, Xie Xiaojun, Liu Shixiang, Wang Yibo, Song Shuang, Wang Long, Guo Jia, Sun Rui, 2018. Structural Patterns of Thrust-Related Folds of Deepwater Fold and Thrust Belts in NW Borneo. Earth Science, 43(2): 491-501. doi: 10.3799/dqkx.2018.024

PDF( 5574 KB)

Structural Patterns of Thrust-Related Folds of Deepwater Fold and Thrust Belts in NW Borneo

doi: 10.3799/dqkx.2018.024

CNOOC Research Institute Ltd., Beijing 100028, China

Received Date: 2017-12-27
Publish Date: 2018-02-15

Abstract

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.
- deepwater fold and thrust belt,
- thrust structure,
- anticline,
- structural style,
- NW Borneo,
- South China Sea,
- petroleum geology

FullText(HTML)

References(52)

References

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

Bugge, T., 1983.Submarine Slides on the Norwegian Continental Margin, with Special Emphasis on the Storegga Area (Dissertation).Continental Shelf Institute, Trondheim, 110-152.

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

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).

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

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

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)

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

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

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

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

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

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

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

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

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

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

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

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

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.

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

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

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.

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

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

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

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

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

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

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

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

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

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

Morley, C.K., 2009.Growth of Folds in a Deep-Water Setting.Geosphere, 5(2):59-89. https://doi.org/10.1130/ges00186.1

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

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

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

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

Petronas, 1999.The Petroleum Geology and Resources of Malaysia.Petoliam Nasional Berhad, Kuala Lumpur.

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.

Sandal, S.T., 1996.The Geology and Hydrocarbon Resources of Negara Brunei Darussalam.Brunei Shell Petroleum Company/Brunei Museum, Syabas Bandar Seri Begawan.

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.

Sloan, E.D., Koh, C.A., 1990.Clatherate Hydrates of Natural Gases.CRC Press, Boca Raton.

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.

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..

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

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

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

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

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

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

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

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(8)

Get Citation

PDF

XML

Article views (3104) PDF downloads(20)

Structural Patterns of Thrust-Related Folds of Deepwater Fold and Thrust Belts in NW Borneo

doi: 10.3799/dqkx.2018.024

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content