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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 劉家瑄 | |
dc.contributor.author | Liang-Fu Lin | en |
dc.contributor.author | 林亮甫 | zh_TW |
dc.date.accessioned | 2021-06-16T17:45:18Z | - |
dc.date.available | 2021-03-02 | |
dc.date.copyright | 2020-03-02 | |
dc.date.issued | 2020 | |
dc.date.submitted | 2020-02-27 | |
dc.identifier.citation | Armentrout, J.M., 1991. Paleontologic Constraints on Depositional Modeling: Examples of Integration of Biostratigraphy and Seismic Stratigraphy, Pliocene-Pleistocene, Gulf of Mexico. In: Weimer, P., Link, M.H. (Eds.), Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems, Frontiers in Sedimentary Geology. Springer, New York, NY, 137–170. https://doi.org/10.1007/978-1-4684-8276-8_7
Badalini, G., Kneller, B., Winker, C.D., 2000. Architecture and processes in the late Pleistocene Brazos-Trinity turbidite system, Gulf of Mexico continental slope. In: Deep-Water Reservoirs of the World: SEPM, Gulf Coast Section, 20th Annual Research Conference. 16–34. Bouma, A.H., 2004. Key controls on the characteristics of turbidite systems. In: Lomas, S.A., Joseph, P. (Eds.), Confined Turbidite Systems. Geological Society 9–22. Bouma, A.H., 2000. Coarse-grained and fine-grained turbidite systems as end member models: applicability and dangers. Marine and Petroleum Geology 17, 137–143. https://doi.org/10.1016/S0264-8172(99)00020-3 Bowin, C., Lu, R.S., Lee, C.-S., Schouten, H., 1978. Plate Convergence and Accretion in Taiwan-Luzon Region. AAPG Bulletin 62, 1645–1672. 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, 6299–6328. https://doi.org/10.1029/92JB02280 Catuneanu, O., 2006. Principles of Sequence Stratigraphy. Elsevier. Amsterdam. 375 p. Catuneanu, O., Galloway, W.E., Kendall, C.G.S.C., Miall, A.D., Posamentier, H.W., Strasser, A., Tucker, M.E., 2011. Sequence stratigraphy: methodology and nomenclature. Newsletters on stratigraphy 44, 173–245. Chen, W.-S., Ridgway, K.D., Horng, C.-S., Chen, Y.-G., Shea, K.-S., Yeh, M.-G., 2001. Stratigraphic architecture, magnetostratigraphy, and incised-valley systems of the Pliocene-Pleistocene collisional marine foreland basin of Taiwan. Geological Society of America Bulletin 113(10), 1249-1271. Chiang, C.-S., Yu, H.-S., 2006. Morphotectonics and incision of the Kaoping submarine canyon, SW Taiwan orogenic wedge. Geomorphology 80, 199–213. https://doi.org/10.1016/j.geomorph.2006.02.008 Chronology of Fluctuating Sea Levels Since the Triassic. Science 235(4793), 1156-1167. Clark, I.R., Cartwright, J.A., 2011. Key controls on submarine channel development in structurally active settings. Marine and Petroleum Geology 28, 1333–1349. https://doi.org/10.1016/j.marpetgeo.2011.02.001 Clark, I.R., Cartwright, J.A., 2009. Interactions between submarine channel systems and deformation in deepwater fold belts: Examples from the Levant Basin, Eastern Mediterranean Sea. Marine and Petroleum Geology 26, 1465–1482. https://doi.org/10.1016/j.marpetgeo.2009.05.004 Clift, P., Gaedicke, C., Edwards, R., Lee, J.I., Hildebrand, P., White, R.S., Schlüter, H.-U., 2002. The stratigraphic evolution of the Indus Fan and the history of sedimentation in the Arabian Sea. Marine Geophysical Researches 23(3), 223-245. 23. Clift, P., Lin, J., 2001. Preferential mantle lithospheric extension under the South China margin. Marine and Petroleum Geology 18, 929–945. https://doi.org/10.1016/S0264-8172(01)00037-X Dadson, S.J., Hovius, N., Chen, H., Dade, W.B., Hsieh, M.-L., Willett, S.D., Hu, J.-C., Horng, M.-J., Chen, M.-C., Stark, C.P., Lague, D., Lin, J.-C., 2003. Links between erosion, runoff variability and seismicity in the Taiwan orogen. Nature 426, 648–651. https://doi.org/10.1038/nature02150 Deptuck, M.E., Steffens, G.S., Barton, M., Pirmez, C., 2003. Architecture and evolution of upper fan channel-belts on the Niger Delta slope and in the Arabian Sea. Marine and Petroleum Geology 20, 649–676. https://doi.org/10.1016/j.marpetgeo.2003.01.004 Dickinson, W.R., Seely, D.R., 1979. Structure and Stratigraphy of Forearc Regions. AAPG Bulletin 63, 2–31. https://doi.org/10.1306/C1EA55AD-16C9-11D7-8645000102C1865D Dickinson, W.R., Suczek, C.A., 1979. Plate Tectonics and Sandstone Compositions. AAPG Bulletin 63, 2164–2182. https://doi.org/10.1306/2F9188FB-16CE-11D7-8645000102C1865D Ding, W., Li, J., Han, X., Suess, E., Huang, Y., Qiu, X., Li, M., 2010. Morphotectonics and formation of the Taiwan Bank Canyon, Southwest offshore Taiwan Island. J Oceanogr Mar Sci 14(4), 65-78. Ding, W., Li, J., Li, M., Qiu, X., Fang, Y., Tang, Y., 2008. A Cenozoic tectono-sedimentary model of the Tainan Basin, the South China Sea: evidence from a multi-channel seismic profile. J. Zhejiang Univ. Sci. A 9, 702–713. https://doi.org/10.1631/jzus.A071572 Flood, R.D., 1988. A lee wave model for deep-sea mudwave activity. Deep Sea Research Part A. Oceanographic Research Papers 35, 973–983. https://doi.org/10.1016/0198-0149(88)90071-4 Flood, R.D., Manley, P.L., Kowsmann, R.O., Appi, C.J., Pirmez, C., 1991. Seismic Facies and Late Quaternary Growth of Amazon Submarine Fan, in: Weimer, P., Link, M.H. (Eds.), Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems, Frontiers in Sedimentary Geology. Springer, New York, NY, 415–433. https://doi.org/10.1007/978-1-4684-8276-8_23 Flood, R.D., Piper, D.J.W., Klaus, A., Peterson, L.C. (Eds.), 1997. Proceedings of the Ocean Drilling Program, 155 Scientific Results, Proceedings of the Ocean Drilling Program. Ocean Drilling Program. https://doi.org/10.2973/odp.proc.sr.155.1997 Fuh, S.-C., Wu, M.-S., Liu, C.-S., 1997. Migration of canyon system from Pliocene to Pleistocene in area between Hsyning structure and Kaoping slope and its application for hydrocarbon exploration. Petroleum Geology of Taiwan 31, 43–60. Fuh, S.-C., Liang, S.-C., Wu, M.-S., 2004a. Spatial and temporal evolution of the Plio-Pleistocene submarine Canyons between Potzu and Tainan, Taiwan. Petroleum Geology of Taiwan 36, 1–18. Fuh, S.-C., Chern, C.-C., Liang, S.-C., Yang, Y.-L., Wu, S.-H., Chang, T.-Y., Lin, J.-Y., 2009. The biogenic gas potential of the submarine canyon systems of Plio-Peistocene foreland Basin, southwestern Taiwan. Marine and Petroleum Geology 26, 1087–1099. https://doi.org/10.1016/j.marpetgeo.2008.09.007 Gong, C., Wang, Y., Peng, X., Li, W., Qiu, Y., Xu, S., 2012. Sediment waves on the South China Sea Slope off southwestern Taiwan: Implications for the intrusion of the Northern Pacific Deep Water into the South China Sea. Marine and Petroleum Geology 32, 95–109. https://doi.org/10.1016/j.marpetgeo.2011.12.005 Gong, C., Wang, Y., Xu, S., Pickering, K.T., Peng, X., Li, W., Yan, Q., 2015. The northeastern South China Sea margin created by the combined action of down-slope and along-slope processes: Processes, products and implications for exploration and paleoceanography. Marine and Petroleum Geology 64, 233–249. https://doi.org/10.1016/j.marpetgeo.2015.01.016 Graham, S.A., Dickinson, W.R., Ingersoll, R.V., 1975. Himalayan-Bengal Model for Flysch Dispersal in the Appalachian-Ouachita System. GSA Bulletin 86, 273–286. https://doi.org/10.1130/0016-7606(1975)86<273:HMFFDI>2.0.CO;2 Hamilton, E.L., 1980. Geoacoustic modeling of the sea floor. The Journal of the Acoustical Society of America 68, 1313–1340. https://doi.org/10.1121/1.385100 Haq, B.U., Hardenbol, J., Vail, P.R., 1987. Chronology of Fluctuating Sea Levels Since the Triassic. Science 235, 1156–1167. https://doi.org/10.1126/science.235.4793.1156 Heiniö, P., Davies, R.J., 2007. Knickpoint migration in submarine channels in response to fold growth, western Niger Delta. Marine and Petroleum Geology 24 (6-9), 434–449. https://doi.org/10.1016/j.marpetgeo.2006.09.002 Ho, C.S., 1986. A synthesis of the geologic evolution of Taiwan. Tectonophysics, 125 (1-3), 1–16. https://doi.org/10.1016/0040-1951(86)90004-1 Hsiung, K.-H., Yu, H.-S., 2013. Sediment dispersal system in the Taiwan–South China Sea collision zone along a convergent margin: A comparison with the Papua New Guinea collision zone of the western Solomon Sea. Journal of Asian Earth Sciences 62, 295–307. https://doi.org/10.1016/j.jseaes.2012.10.006 Hsiung, K.-H., Yu, H.-S., Chiang, C.-S., 2014. Seismic characteristics, morphology and formation of the ponded Fangliao Fan off southwestern Taiwan, northern South China Sea. Geo-Mar Lett 34, 59–74. https://doi.org/10.1007/s00367-013-0351-1 Hsiung, K.-H., Yu, H.-S., Su, M., 2015. Sedimentation in remnant ocean basin off SW Taiwan with implication for closing northeastern South China Sea. Journal of the Geological Society 172, 641–647. https://doi.org/10.1144/jgs2014-077 Huang, C.-Y., Yuan, P.B., Lin, C.-W., Wang, T.K., Chang, C.-P., 2000. Geodynamic processes of Taiwan arc–continent collision and comparison with analogs in Timor, Papua New Guinea, Urals and Corsica. Tectonophysics 325, 1–21. https://doi.org/10.1016/S0040-1951(00)00128-1 Huh, C.-A., Lin, H.-L., Lin, S., Huang, Y.-W., 2009. Modern accumulation rates and a budget of sediment off the Gaoping (Kaoping) River, SW Taiwan: A tidal and flood dominated depositional environment around a submarine canyon. Journal of Marine Systems 76, 405–416. https://doi.org/10.1016/j.jmarsys.2007.07.009 Ingersoll, R.V., Graham, S.A., Dickinson, W.R., 1995. Remnant ocean basins. In: Busty, C.J., Ingersoll, R.V. (eds), Tectonics of Sedimentary Basins. Blackwell Science, Oxford, 363–391. Kalbas, J.L., Ridgway, K.D., Gehrels, G.E., Trop, J.M., Glen, J.M.G., O’neill, J.M., 2007. Stratigraphy, depositional systems, and provenance of the Lower Cretaceous Kahiltna assemblage, western Alaska Range: Basin development in response to oblique collision. Geological Society of America Special Papers 431, 307-343. Kneller, B., 2003. The influence of flow parameters on turbidite slope channel architecture. Marine and Petroleum Geology 20, 901–910. https://doi.org/10.1016/j.marpetgeo.2003.03.001 Lallemand, S.E., Tsien, H.-H., 1997. An introduction to active collision in Taiwan. Tectonophysics 274, 1–4. https://doi.org/10.1016/S0040-1951(96)00294-6 Li, C.-F., Xu, X., Lin, J., Sun, Z., Zhu, J., Yao, Y., Zhao, X., Liu, Q., Kulhanek, D.K., Wang, J., Song, T., Zhao, J., Qiu, N., Guan, Y., Zhou, Z., Williams, T., Bao, R., Briais, A., Brown, E.A., Chen, Y., Clift, P.D., Colwell, F.S., Dadd, K.A., Ding, W., Almeida, I.H., Huang, X.-L., Hyun, S., Jiang, T., Koppers, A.A.P., Li, Q., Liu, C., Liu, Z., Nagai, R.H., Peleo‐Alampay, A., Su, X., Tejada, M.L.G., Trinh, H.S., Yeh, Y.-C., Zhang, C., Zhang, F., Zhang, G.-L., 2014. Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349. Geochemistry, Geophysics, Geosystems 15, 4958–4983. https://doi.org/10.1002/2014GC005567 Li, C.-F., Zhou, Z., Li, J., Hao, H., Geng, J., 2007. Structures of the northeasternmost South China Sea continental margin and ocean basin: geophysical constraints and tectonic implications. Mar Geophys Res 28, 59–79. https://doi.org/10.1007/s11001-007-9014-9 Liao, W.-Z., Lin, A.T., Liu, C.-S., Oung, J.-N., Wang, Y., 2016. A study on tectonic and sedimentary development in the rifted northern continental margin of the South China Sea near Taiwan. Interpretation 4, 47–65. https://doi.org/10.1190/INT-2015-0209.1 Lin, A.T., Liu, C.-S., Lin, C.-C., Schnurle, P., Chen, G.-Y., Liao, W.-Z., Teng, L.S., Chuang, H.-J., Wu, M.-S., 2008. Tectonic features associated with the overriding of an accretionary wedge on top of a rifted continental margin: An example from Taiwan. Marine Geology 255, 186–203. https://doi.org/10.1016/j.margeo.2008.10.002 Lin, A.T., Yao, B., Hsu, S.-K., Liu, C.-S., Huang, C.-Y., 2009. Tectonic features of the incipient arc-continent collision zone of Taiwan: Implications for seismicity. Tectonophysics 479, 28–42. https://doi.org/10.1016/j.tecto.2008.11.004 Lin, C.-C., Lin, A.T.-S., Liu, C.-S., Horng, C.-S., Chen, G.-Y., Wang, Y., 2014. Canyon-infilling and gas hydrate occurrences in the frontal fold of the offshore accretionary wedge off southern Taiwan. Mar Geophys Res 35, 21–35. https://doi.org/10.1007/s11001-013-9203-7 Liu, C.-S., Deffontaines, B., Lu, C.-Y., Lallemand, S., 2004. Deformation Patterns of an Accretionary Wedge in the Transition Zone from Subduction to Collision Offshore Southwestern Taiwan. Mar Geophys Res 25, 123–137. https://doi.org/10.1007/s11001-005-0738-0 Liu, C.-S., Huang, I.L., Teng, L.S., 1997. Structural features off southwestern Taiwan. Marine Geology 137, 305–319. https://doi.org/10.1016/S0025-3227(96)00093-X Liu, C.-S., Lundberg, N., Reed, D.L., Huang, Y.-L., 1993. Morphological and seismic characteristics of the Kaoping Submarine Canyon. Marine Geology 111, 93–108. https://doi.org/10.1016/0025-3227(93)90190-7 Liu, J.T., Huh, C.A., You, C.-F., 2009. Fate of Terrestrial Substances in the Gaoping (Kaoping) Shelf/Slope and in the Gaoping Submarine Canyon off SW Taiwan. Journal of Marine System 76, 367–368. https://doi.org/10.1016/j.jmarsys.2008.08.005 MARGINS Science Plans, 2004. http://margins.wustl.edu/Publications/SciencePlans/MARGINSSciencePlans.html Mayall, M., Jones, E., Casey, M., 2006. Turbidite channel reservoirs—Key elements in facies prediction and effective development. Marine and Petroleum Geology 23, 821–841. https://doi.org/10.1016/j.marpetgeo.2006.08.001 Mitchell, N.C., 2006. Morphologies of knickpoints in submarine canyons. Geological Society of America Bulletin 118, 589–605. https://doi.org/10.1130/B25772.1 Mitchum, R.M., Vail, P.R., Sangree, J.B., 1977. Seismic Stratigraphy and Global Changes of Sea Level: Part 6. Stratigraphic Interpretation of Seismic Reflection Patterns in Depositional Sequences. In: Payton, C.E. (ed), Seismic Stratigraphy- applications to hydrocarbon exploration. AAPG Memoir 26, 117–133. Morley, C.K., 2016. Major unconformities/termination of extension events and associated surfaces in the South China Seas: Review and implications for tectonic development. Journal of Asian Earth Sciences 120, 62–86. https://doi.org/10.1016/j.jseaes.2016.01.013 Nichols, G., 2009. Sedimentology and Stratigraphy. Wiley-Blackwell. 419 p. Posamentier, H.W., Kolla, V., 2003. Seismic Geomorphology and Stratigraphy of Depositional Elements in Deep-Water Settings. Journal of Sedimentary Research 73, 367–388. https://doi.org/10.1306/111302730367 Reading, H.G., Richards, M., 1994. Turbidite Systems in Deep-Water Basin Margins Classified by Grain Size and Feeder System. AAPG Bulletin 78, 792–822. https://doi.org/10.1306/A25FE3BF-171B-11D7-8645000102C1865D Reed, D.L., Lundberg, N., Liu, C.-S., Kuo, B.-Y., 1992. Structural Relations along the Margins of the Offshore Taiwan Accrentionary Wedge:Implications for Accretion and Crustal Kinematics. Acta Gelological Taiwanica 30, 105–122. Ru, K., Pigott, J.D., 1986. Episodic Rifting and Subsidence in the South China Sea. AAPG Bulletin 70, 1136–1155. Salles, L., Ford, M., Joseph, P., 2014. Characteristics of axially-sourced turbidite sedimentation on an active wedge-top basin (Annot Sandstone, SE France). Marine and Petroleum Geology 56, 305–323. https://doi.org/10.1016/j.marpetgeo.2014.01.020 Schwenk, T., Spieß, V., Hübscher, C., Breitzke, M., 2003. Frequent channel avulsions within the active channel–levee system of the middle Bengal Fan—an exceptional channel–levee development derived from Parasound and Hydrosweep data. Deep Sea Research Part II: Topical Studies in Oceanography, Bay of Bengal 50, 1023–1045. https://doi.org/10.1016/S0967-0645(02)00618-5 Shanmugam, G., 2016. Submarine fans: A critical retrospective (1950–2015). Journal of Palaeogeography 5, 110–184. https://doi.org/10.1016/j.jop.2015.08.011 Shanmugam, G., Moiola, R.J., 1988. Submarine fans: Characteristics, models, classification, and reservoir potential. Earth-Science Reviews 24, 383–428. https://doi.org/10.1016/0012-8252(88)90064-5 Stow, D.A.V., Howell, D.G., Nelson, C.H., 1983. Sedimentary, tectonic, and sea-level controls on submarine fan and slope-apron turbidite systems. Geo-Marine Letters 3, 57–64. https://doi.org/10.1007/BF02462448 Stow, D.A.V., Mayall, M., 2000. Deep-water sedimentary systems: New models for the 21st century. Marine and Petroleum Geology 17, 125–135. https://doi.org/10.1016/S0264-8172(99)00064-1 Samuel, S.P., 2010. Depositional History of Paleocene Sediments in the Offshore Canterbury Basin, New Zealand. Master thesis. Victoria University of Wellington. Su, C.-C., Hsu, S.-T., Hsu, H.-H., Lin, J., Dong, J.-J., 2018. Sedimentological characteristics and seafloor failure offshore SW Taiwan. Terr. Atmos. Ocean. Sci. 29 (1), 65-76. https://doi.org/10.3319/tao.2017.06.21.01 Su, C.-C., Tseng, J.-Y., Hsu, H.-H., Chiang, C.-S., Yu, H.-S., Lin, S., Liu, J.T., 2012. Records of submarine natural hazards off SW Taiwan. Geological Society, London, Special Publications 361, 41–60. https://doi.org/10.1144/SP361.5 Su, D., White, N., McKenzie, D., 1989. Extension and subsidence of the Pearl River Mouth Basin, northern South China Sea. Basin Research 2, 205–222. https://doi.org/10.1111/j.1365-2117.1989.tb00036.x Suppe, J., 1984. Kinematics of arc-continent collision, flipping of subduction, and back-arc spreading near Taiwan. Memoir. Geol. Soc. China 6, 21–33. Taylor, B., Hayes, D.E., 1983. Origin and history of the South China Sea basin. The tectonic and geologic evolution of Southeast Asian seas and islands: Part 2 27, 23-56. https://doi.org/10.1029/GM027p0023 Teng, L.S., 1990. Geotectonic evolution of late Cenozoic arc-continent collision in Taiwan. Tectonophysics 183, 57–76. https://doi.org/10.1016/0040-1951(90)90188-E Vail, P.R., Mitchum, R.M., Todd R.G., Widmier J.M., Thompson S., Sangree J.B., Bubb J.N., Hatlelid W.G., 1977. Seismic stratigraphy and global changes of sea level. In: Payton C.E. (ed), Seismic Stratigraphy Applications to Hydrocarbon Exploration. AAPG Memoir 26, 49-212. Wagoner, J.C.V., Posamentier, H.W., Mitchum, R.M., Vail, P.R., Sarg, J.F., Loutit, T.S., Hardenbol, J., 1988. An Overview of the Fundamentals of Sequence Stratigraphy and Key Definitions. SEPM Special Publication 42, 39–45 Weislogel, A.L., Chang, E.Z., Graham, S.A., 2007. Accumulation of the Middle to Upper Triassic Songpan-Ganzi Turbidite Complex, China. In: Nilsen, R.D., Shew, G.S., Steffens G.S., Studlick J.R., (eds), Atlas of Deep-Water Outcrops: AAPG Studies in Geology 56 1-20. https://doi.org/10.1306/12401009St563314 Winker, C.D., 1996. High-Resolution Seismic Stratigraphy of a Late Pleistocene Submarine Fan Ponded by Salt-Withdrawal Mini-Basins on the Gulf of Mexico Continental Slope. Offshore Technology Conference. https://doi.org/10.4043/8024-MS Yang, T.F., Lee, T., Chen, C.-H., Cheng, S.-N., Knittel, U., Punongbayan, R.S., Rasdas, A.R., 1996. A double island arc between Taiwan and Luzon: consequence of ridge subduction. Tectonophysics 258, 85–101. https://doi.org/10.1016/0040-1951(95)00180-8 Yeh, Y.-C., Hsu, S.-K., Doo, W.-B., Sibuet, J.-C., Liu, C.-S., Lee, C.-S., 2012. Crustal features of the northeastern South China Sea: insights from seismic and magnetic interpretations. Mar Geophys Res 33, 307–326. https://doi.org/10.1007/s11001-012-9154-4 Yeh, Y.-C., Sibuet, J.-C., Hsu, S.-K., Liu, C.-S., 2010. Tectonic evolution of the Northeastern South China Sea from seismic interpretation. Journal of Geophysical Research: Solid Earth 115. https://doi.org/10.1029/2009JB006354 Yu, H.-S., Chang, E.T.-Y., 2009. Links among slope morphology, canyon types and tectonics on passive and active margins in the northernmost South China Sea. J. Earth Sci. 20, 77–84. https://doi.org/10.1007/s12583-009-0008-1 Yu, H.-S., Chiang, C.-S., Shen, S.-M., 2009. Tectonically active sediment dispersal system in SW Taiwan margin with emphasis on the Gaoping (Kaoping) Submarine Canyon. Journal of Marine Systems 76, 369–382. https://doi.org/10.1016/j.jmarsys.2007.07.010 Yu, H.-S., Hong, E., 2006. Shifting submarine canyons and development of a foreland basin in SW Taiwan: controls of foreland sedimentation and longitudinal sediment transport. Journal of Asian Earth Sciences 27, 922–932. https://doi.org/10.1016/j.jseaes.2005.09.007 Zhong, G., Cartigny, M.J.B., Kuang, Z., Wang, L., 2015. Cyclic steps along the South Taiwan Shoal and West Penghu submarine canyons on the northeastern continental slope of the South China Sea. Geological Society of America Bulletin 127, 804–824. https://doi.org/10.1130/B31003.1 沈剛年,2017,台灣西南海域之增基岩體於更新世以來受到構造控制之深海水道/深海扇系統演育。國立中央大學地球科學學系,碩士論文,共 84 頁。 林亮甫、劉家瑄、林哲銓、許鶴瀚、陳松春,2016,高屏下部斜坡地質特性與流體系統聲學表現。經濟部中央地質調查所特刊第30號,第 159-180 頁。 林殿順,1991,台灣西南部麓山帶上新-更新統之沈積岩相與沈積環境演化。國立台灣大學地質學研究所,碩士論文,共 93 頁。 陳文山、合信昌、王源、楊昭男、高銘健、張益生、顎中信、陳勉銘,1994,台灣西南部上新統的岩象學研究與地層對比。 經濟部中央地質調查所特刊第8號,第 83-99 頁。 陳文山、俞何興、俞震甫、鍾孫霖、林正洪、林啟文、游能悌、吳逸民、王國龍,2016,臺灣地質概論。中華民國地質學會。共204頁。 陳文山、黃能偉、楊志成,2011,臺灣西南部更新世沈積層序特性與前陸盆地演化。 經濟部中央地質調查所特刊第25號,第 1-38 頁。 潘玉生、陳讚煌、鍾火盛、游銘銳,1992,震測資料之認識與解釋。中國石油股份有限公司海域及海外石油探勘觸及中國地球物理協會,共280頁。 SEPM website http://www.sepmstrata.org/page.aspx?pageid=1 | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/64405 | - |
dc.description.abstract | 台灣造山帶劇烈地抬升,供應了大量的沉積物到周圍的海域,是海底沉積系統發育的良好條件,因此在台灣島周圍可觀察到許多海底峽谷與海底扇形成。在台灣西南海域,西側是張裂後的南海被動大陸邊緣,東側則是因板塊聚合作用形成的擠壓構造帶,除了在兩側能形成不同類型的沉積系統之外,海盆中更記錄了造山帶的歷史、被動邊緣轉換成活動邊緣過程對沉積作用的影響。然而,在褶皺帶的地層受到變形、侵蝕、變質作用,幾乎無法探究過去發育的沉積系統的全貌,使得許多在造山過程中留下的地質資訊不易解讀,甚至被忽略。本研究利用多頻道反射震測資料配合層面拉平技術探討在下部高屏斜坡褶皺帶變形的地層特徵,並在此辨識出了兩個大範圍分布的海底扇-由澎湖峽谷生成的澎湖扇與由高屏峽谷生成的高屏扇。本研究進一步透過震測相分析,探討此兩海底扇的基本性質與演化,也嘗試將這兩個海底扇的特性與演化對應到它們上游的地層紀錄,探討當時造就澎湖扇與高屏扇的沉積物散布系統,以及影響這兩個系統的沉積物特性、構造與海水面變化等因素。
研究結果顯示澎湖扇是由單點供應的多期自然堤水道組成的長型海底扇,具有細顆粒海底扇的特徵。由當時的濁水溪供給造山帶沉積物到前陸盆地的海底峽谷中向南傳輸,最終在下部高屏斜坡堆出澎湖扇,是一個在被動邊緣與活動邊緣間的沉積物散布系統,稱為澎湖系統。高屏扇則是由單點供應的多期砂體堆覆而成的舌狀海底扇,具有偏粗顆粒海底扇的特徵。由當時的高屏溪供給造山帶沉積物進到旗山斷層上盤的背負盆地中,供應至在活動邊緣下切的高屏峽谷上段,再經過平行構造發育的高屏峽谷中段向南輸送,最終在下部高屏斜坡堆出高屏扇,是一個在活動邊緣上的沉積物散布系統,稱為高屏系統。這兩個系統發育的地點與特性都受到構造演化的控制,而在下部高屏斜坡的褶皺構造形成以後,兩條海底峽谷都向西南切過構造帶,在構造帶上的沉積作用改變,沿著峽谷流徑輸送的沉積物在構造高區以掠過為主、在背負盆地中常從峽谷溢出而滯留在褶皺帶上。澎湖扇具有反映海水面循環的特徵,其中辨識出的五個層序邊界似乎與台南一帶辨識出的層序邊界具有類似的變化趨勢,具對比的可能性,而澎湖扇的震測相組合可能與本地的海水面變化有關。 澎湖扇與高屏扇相較於世界各地發育的海底扇規模並不算大,但是若考量台灣造山帶的規模,兩扇體總和面積超過現代台灣島面積的六分之一,體積更是大約現代台灣島體積的三分之一,是一個弧陸碰撞造成的殘餘海盆中顯著的沉積物聚集。 | zh_TW |
dc.description.abstract | The Taiwan orogen, known for its highest erosion rate in the world, discharges voluminous sediments into the nearby ocean basins. During the processes, submarine canyons and fans were developed around Taiwan. In the area off southwest Taiwan, the rift margin of northeastern South China Sea lies in the west and convergent complex of Taiwan orogen develops in the east, the depositional systems have been developed under different tectonic controls on both sides. This area should preserve the sedimentary records of both the passive margin and active margin settings, and also the depositional transformation between the two tectonic settings as the orogeny propagates westward. However, as the sedimentary layers are deformed, eroded, or even metamorphosed in the convergent zone, the stratigraphic characteristics are difficult to be recognized and often being ignored. In this study, the marine seismic reflection data were used for exploring the stratigraphic characteristics of the lower Gaoping Slope where the folded strata are finely imaged. To better understand the deformed depositional features, the “horizon flattening” technique was applied to present the depositional elements. In the study area, two depositional systems with different characteristics have been identified, namely the Penghu Fan and Gaoping Fan. Based on seismic facies analyses, their respective properties and temporal and spatial variations are discussed. These observations are correlated to the stratigraphic characteristics in their upstream area for discussing their respective sediment dispersal systems and the controlling factors of the sediment properties, structural activities and sea-level fluctuations.
The Penghu Fan is a point-source elongate submarine fan characterized by lobe-channel-levee complexes presenting its fine-grained nature. Formed between the passive and active margins, its sediment dispersal system, the Penghu System, comprised by ancient Choshui River and submarine canyons proximally in the foreland basin and distally on the slope area. On the other hand, the Gaoping fan is a point-source lobate submarine fan characterized by stacked sandy deposits presenting its coarser-grain nature. Formed on the active margin, its sediment dispersal system, the Gaoping System, comprised by the ancient Gaoping river on the hanging-wall piggyback basin of the Chishan fault and the submarine canyon on the uplifted slope (the Upper Gaoping Slope ). The courses and properties of both systems are controlled by tectonic settings. Since fold belt is developed in the Lower Gaoping Slope, the Penghu and Gaoping Fans are deformed and uplifted, and both Penghu and Gaoping Canyons tend to cut across the fold belt and terminally connect to the trough along the deformation front, rather than developing along the piggyback basins on the active slope. During this period, the sediments transporting along the canyons either bypass the structural highs or being spilled into the piggyback basins formed on the slope. Cyclic depositional pattern in Penghu Fan is observed, suggesting the development of Penghu Fan could be related to local sea-level fluctuations. Five identified sequence boundaries are present in both the Penghu Fan and its upstream area. The depositional trends are similar, so these sequence boundaries are suggested to be correlated. The development of Gaoping Fan is probably also related to the sea-level fluctuations, but it does not show a distinct cyclic pattern. This may reflect the system on active margin is more controlled by structural events. Comparing to other submarine fans reported, the sizes of Penghu and Gaoping Fans are moderate. However, if the size of the sediment source provenance (the Taiwan Orogen) is taken into consideration, the area of Penghu and Gaoping Fans is larger than 1/6 of the modern Taiwan Island, and the total volume is about 1/3 of the modern Taiwan Island. These two submarine fans present significant sediment accumulation in a remnant ocean basin; thus the Penghu and Gaoping Fans could be a representative case of the remnant ocean submarine fans in an arc-continental collision setting. | en |
dc.description.provenance | Made available in DSpace on 2021-06-16T17:45:18Z (GMT). No. of bitstreams: 1 ntu-109-F00241318-1.pdf: 24050853 bytes, checksum: 2fe1128c7d349c7c47f3951582737876 (MD5) Previous issue date: 2020 | en |
dc.description.tableofcontents | 誌謝 i
摘要 ii Abstract iv 目錄 vii 圖目錄 ix 表目錄 xii 第一章 緒論 1 1.1 前言 1 1.2 海底扇的特徵與控制因素 3 1.3 研究區域與地質背景 10 1.4 前人研究與研究動機 18 第二章 研究資料與方法 24 2.1 海域多頻道反射震測資料 24 2.2 震測地層學 31 2.3 層面拉平 37 第三章 下部高屏斜坡的震測相與層序 39 3.1 構造與地層架構 39 3.2 震測相解釋 45 3.3 層序分析 49 3.4 層序解釋 72 第四章 結果與討論 85 4.1 澎湖扇與高屏扇的沉積特徵與震測相組合 85 4.2 澎湖系統 87 4.3 高屏系統 102 4.4 澎湖與高屏海底扇規模 106 4.5 本研究結果與過去研究對澎湖、高屏系統研究認知上的異同 110 4.6 構造因素與沉積物性質對台灣西南海域海底扇發育的影響 112 4.7 海底扇震測相組合與深海層序地層學 114 第五章 結論 118 參考文獻 120 | |
dc.language.iso | zh-TW | |
dc.title | 台灣西南海域澎湖與高屏海底扇系統之沉積震測特徵 | zh_TW |
dc.title | Depositional elements and seismic characteristics of the Penghu and Gaoping submarine fan systems off SW Taiwan | en |
dc.type | Thesis | |
dc.date.schoolyear | 108-1 | |
dc.description.degree | 博士 | |
dc.contributor.oralexamcommittee | 鄧屬予,吳榮章,陳文山,林殿順,楊耿明 | |
dc.subject.keyword | 海底扇,沉積物散布系統,多頻道反射震測,台灣西南海域,高屏扇,澎湖扇, | zh_TW |
dc.subject.keyword | submarine fan,sediment dispersal system,multi-channel seismic reflection data,off southwestern Taiwan,Gaoping Fan,Penghu Fan, | en |
dc.relation.page | 131 | |
dc.identifier.doi | 10.6342/NTU202000637 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2020-02-27 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 海洋研究所 | zh_TW |
顯示於系所單位: | 海洋研究所 |
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