請用此 Handle URI 來引用此文件:
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/18541
完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 陳于高 | |
dc.contributor.author | Shao-Yi Huang | en |
dc.contributor.author | 黃韶怡 | zh_TW |
dc.date.accessioned | 2021-06-08T01:10:42Z | - |
dc.date.copyright | 2014-08-21 | |
dc.date.issued | 2014 | |
dc.date.submitted | 2014-08-17 | |
dc.identifier.citation | Andersen, T., 2002, Correction of common lead in U–Pb analyses that do not report 204Pb: Chemical Geology, v. 192, no. 1–2, p. 59-79.
Armijo, R., Tapponnier, P., Mercier, J. L., and Han, T.-L., 1986, Quaternary extension in Southern Tibet: Field observation and tectonic implications: J. Geophys. Res., v. 91. Bernet, M., Brandon, M. T., Garver, J. I., and Molitor, B., 2004, Downstream Changes of Alpine Zircon Fission-Track Ages in the Rhone and Rhine Rivers: Journal of Sedimentary Research, v. 74, no. 1, p. 82-94. Blisniuk, P. M., Hacker, B. R., Glodny, J., Ratschbacher, L., Bi, S., Wu, Z., McWilliams, M. O., and Calvert, A., 2001, Normal faulting in central Tibet since at least 13.5 Myr ago: Nature, v. 412, no. 6847, p. 628-632. Brandon, M. T., 1992, Decomposition of fission-track grain-age distributions: American Journal of Science, v. 292, no. 8, p. 535-564. -, 1996, Probability density plot for fission-track grain-age samples: Radiation Measurements, v. 26, no. 5, p. 663-676. Braun, J., 2005, Quantitative Constraints on the Rate of Landform Evolution Derived from Low-Temperature Thermochronology: Reviews in Mineralogy and Geochemistry, v. 58, no. 1, p. 351-374. Brewer, I. D., Burbank, D. W., and Hodges, K. V., 2003, Modelling detrital cooling-age populations: insights from two Himalayan catchments: Basin Research, v. 15, no. 3, p. 305-320. -, 2006, Downstream development of a detrital cooling-age signal: Insights from Ar-40/Ar-39 muscovite thermochronology in the Nepalese Himalaya, in Willett, S. D., Hovius, N., Brandon, M. T., and Fisher, D. M., eds., Tectonics, Climate, and Landscape Evolution, Volume 398: Boulder, Geological Soc Amer Inc, p. 321-338. Chiu, H.-Y., Chung, S.-L., Wu, F.-Y., Liu, D., Liang, Y.-H., Lin, I. J., Iizuka, Y., Xie, L.-W., Wang, Y., and Chu, M.-F., 2009, Zircon U–Pb and Hf isotopic constraints from eastern Transhimalayan batholiths on the precollisional magmatic and tectonic evolution in southern Tibet: Tectonophysics, v. 477, no. 1–2, p. 3-19. Chung, S.-L., Chu, M.-F., Ji, J., O'Reilly, S. Y., Pearson, N. J., Liu, D., Lee, T.-Y., and Lo, C.-H., 2009, The nature and timing of crustal thickening in Southern Tibet: Geochemical and zircon Hf isotopic constraints from postcollisional adakites: Tectonophysics, v. 477, no. 1-2, p. 36-48. Cina, S. E., Yin, A., Grove, M., Dubey, C. S., Shukla, D. P., Lovera, O. M., Kelty, T. K., Gehrels, G. E., and Foster, D. A., 2009, Gangdese arc detritus within the eastern Himalayan Neogene foreland basin: Implications for the Neogene evolution of the Yalu-Brahmaputra River system: Earth and Planetary Science Letters, v. 285, no. 1-2, p. 150-162. Coleman, M., and Hodges, K., 1995, Evidence for Tibetan plateau uplift before 14 Myr ago from a new minimum age for east–west extension: Nature, v. 374, p. 49-52. Copeland, P., Harrison, T. M., Yun, P., Kidd, W. S. F., Roden, M., and Yuquan, Z., 1995, Thermal evolution of the Gangdese batholith, southern Tibet: A history of episodic unroofing: Tectonics, v. 14. Copeland, P., Mark Harrison, T., Kidd, W. S. F., Xu, R., and Zhang, Y., 1987, Rapid early Miocene acceleration of uplift in the Gangdese Belt, Xizang (southern Tibet), and its bearing on accommodation mechanisms of the India-Asia collision: Earth and Planetary Science Letters, v. 86, no. 2-4, p. 240-252. Dewey, J. F., Shackleton, R. M., Chengfa, C., and Yiyin, S., 1988, The Tectonic Evolution of the Tibetan Plateau: Philosophical Transactions of the Royal Society of London, v. A 327, p. 379-413. Fielding, E., Isacks, B., Barazangi, M., and Duncan, C., 1994, How flat is Tibet?: Geology, v. 22, no. 2, p. 163-167. Fielding, E. J., 1996, Tibet uplift and erosion: Tectonophysics v. 260, no. 1-3, p. 55-84. Finnegan, N. J., Hallet, B., Montgomery, D. R., Zeitler, P. K., Stone, J. O., Anders, A. M., and Yuping, L., 2008, Coupling of rock uplift and river incision in the Namche Barwa Gyala Peri massif, Tibet: Geol Soc Am Bull, v. 120, no. 1-2, p. 142-155. Fleischer, R. L., Price, P. B., and Walker, R. M., 1975, Nuclear tracks in solids. Principles and Applications, Medium: X; Size: Pages: 624 p.: Garver, J. I., Brandon, M. T., Roden-Tice, M., and Kamp, P. J. J., 1999, Erosional denudation determined by fission-track ages of detrital apatite and zircon, in Ring, U., Brandon, M. T., Willett, S., and Lister, G., eds., Exhumation Processes: Normal Faulting, Ductile Flow, and Erosion, Volume 154, Geological Society of London Special Publication, p. 283–304. Garzanti, E., Vezzoli, G., Ando, S., France-Lanord, C., Singh, S. K., and Foster, G., 2004, Sand petrology and focused erosion in collision orogens: the Brahmaputra case: Earth and Planetary Science Letters, v. 220, no. 1-2, p. 157-174. Geng, Q., Guitang, P., Zheng, L., Chen, Z., Fisher, R. D., Sun, Z., Ou, C., Dong, H., Wang, X., Li, S., Lou, X., and Fu, H., 2006, The Eastern Himalayan syntaxis: major tectonic domains, ophiolitic melanges and geologic evolution: Journal of Asian Earth Sciences, v. 27, no. 3, p. 265-285. Griffin, W. L., Belousova, E. A., Shee, S. R., Pearson, N. J., and O’Reilly, S. Y., 2004, Archean crustal evolution in the northern Yilgarn Craton: U–Pb and Hf-isotope evidence from detrital zircons: Precambrian Research, v. 131, no. 3–4, p. 231-282. Harris, N., 2007, Channel flow and the Himalayan-Tibetan orogen: a critical review: Journal of the Geological Society, v. 164, no. 3, p. 511-523. Harrison, T. M., Copeland, P., Kidd, W. S. F., and Lovera, O. M., 1995, Activation of the Nyainqentanghla Shear Zone: Implications for uplift of the southern Tibetan Plateau: Tectonics, v. 14. Harrison, T. M., Copeland, P., Kidd, W. S. F., and Yin, A., 1992, Raising Tibet: Science, v. 255, no. 5052, p. 1663 - 1670. Ireland, T. R., and Williams, I. S., 2003, Considerations in Zircon Geochronology by SIMS: Reviews in Mineralogy and Geochemistry, v. 53, no. 1, p. 215-241. Lee, H.-Y., Chung, S.-L., Lo, C.-H., Ji, J., Lee, T.-Y., Qian, Q., and Zhang, Q., 2009, Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record: Tectonophysics, v. 477, no. 1-2, p. 20-35. Liu, T.-K., Hsieh, S., Chen, Y.-G., and Chen, W.-S., 2001, Thermo-kinematic evolution of the Taiwan oblique-collision mountain belt as revealed by zircon fission track dating: Earth and Planetary Science Letters, v. 186, no. 1, p. 45-56. Lo, C.-H., Chung, S.-L., Lee, T.-Y., and Wu, G., 2002, Age of the Emeishan flood magmatism and relations to Permian–Triassic boundary events: Earth and Planetary Science Letters, v. 198, no. 3–4, p. 449-458. Najman, Y., 2006, The detrital record of orogenesis: A review of approaches and techniques used in the Himalayan sedimentary basins: Earth Science Reviews, v. 74, no. 1-2, p. 1-72. Pan, Y., Copeland, P., Roden, M. K., Kidd, W. S. F., and Mark Harrison, T., 1993, Thermal and unroofing history of the Lhasa area, Southern Tibet--evidence from apatite fission track thermochronology: International Journal of Radiation Applications and Instrumentation. Part D. Nuclear Tracks and Radiation Measurements, v. 21, no. 4, p. 543-554. Rahl, J. M., Ehlers, T. A., and van der Pluijm, B. A., 2007, Quantifying transient erosion of orogens with detrital thermochronology from syntectonic basin deposits: Earth and Planetary Science Letters, v. 256, no. 1-2, p. 147-161. Reiners, P. W., Campbell, I. H., Nicolescu, S., Allen, C. M., Hourigan, J. K., Garver, J. I., Mattinson, J. M., and Cowan, D. S., 2005, (U-Th)/(He-Pb) double dating of detrital zircons: American Journal of Science, v. 305, no. 4, p. 259-311. Renne, P. R., Swisher, C. C., Deino, A. L., Karner, D. B., Owens, T. L., and DePaolo, D. J., 1998, Intercalibration of standards, absolute ages and uncertainties in 40Ar/39Ar dating: Chemical Geology, v. 145, no. 1–2, p. 117-152. Ruhl, K. W., and Hodges, K. V., 2005, The use of detrital mineral cooling ages to evaluate steady state assumptions in active orogens: An example from the central Nepalese Himalaya: Tectonics, v. 24, no. 4, p. -. Ruiz, G. M. H., Seward, D., and Winkler, W., 2004, Detrital thermochronology – a new perspective on hinterland tectonics, an example from the Andean Amazon Basin, Ecuador: Basin Research, v. 16, no. 3, p. 413-430. Sircombe, K. N., 2004, AgeDisplay: an EXCEL workbook to evaluate and display univariate geochronological data using binned frequency histograms and probability density distributions: Computers & Geosciences, v. 30, no. 1, p. 21-31. Stewart, R. J., Hallet, B., Zeitler, P. K., Malloy, M. A., Allen, C. M., and Trippett, D., 2008, Brahmaputra sediment flux dominated by highly localized rapid erosion from the easternmost Himalaya: Geology, v. 36, no. 9, p. 711-714. Stock, G. M., Ehlers, T. A., and Farley, K. A., 2006, Where does sediment come from? Quantifying catchment erosion with detrital apatite (U-Th)/He thermochronometry: Geology, v. 34, no. 9, p. 725-728. Tapponnier, P., Zhiqin, X., Roger, F., Meyer, B., Arnaud, N., Wittlinger, G., and Jingsui, Y., 2001, Oblique Stepwise Rise and Growth of the Tibet Plateau: Science, v. 294, no. 5547, p. 1671-1677. Vermeesch, P., Miller, D. D., Graham, S. A., De Grave, J., and McWilliams, M. O., 2006, Multimethod detrital thermochronology of the Great Valley Group near New Idria, California: Geological Society of America Bulletin, v. 118, no. 1, p. 210-218. Wagner, G., and Van den Haute, P., 1992, Fission track dating, Kluwer Academic Publishers. Wen, D.-R., Liu, D., Chung, S.-l., Chu, M.-f., Ji, J., Zhang, Q., Song, B., Lee, T.-y., Yeh, M.-w., and Lo, C.-h., 2008, Zircon SHRIMP U–Pb ages of the Gangdese Batholith and implications for Neotethyan subduction in southern Tibet: Chemical Geology, v. 252, p. 191-201. Williams, H., Turner, S., Kelley, S., and Harris, N., 2001, Age and composition of dikes in Southern Tibet: New constraints on the timing of east-west extension and its relationship to postcollisional volcanism: Geology, v. 29, no. 4, p. 339-342. Yin, A., 2000, Mode of Cenozoic east-west extension in Tibet suggesting a common origin of rifts in Asia during the Indo-Asian collision: J. Geophys. Res., v. 105, no. B9, p. 21745-21759. -, 2006, Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation: Earth Science Reviews, v. 76, no. 1-2, p. 1-131. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/18541 | - |
dc.description.abstract | 利用沉積物的組成與年代特性,我們可以推論其源區歷史以及集水區的地表地形作用。在此研究中我們使用一序列由低溫至高溫的熱定年學方法(核飛跡定年、氩氩定年、鈾鉛定年),選用適當之標的礦物(鋯石、磷灰石、鉀長石),針對現生河砂沉積物進行分析研究,由結果的熱年代頻譜分布圖我們可以探討集水區的地表作用強度以及分布差異。
本研究選定西藏南部雅魯藏布江的兩條大支流(拉薩河以及尼洋河)進行探討,在這兩條支流的河口所取樣的河砂標本,其鋯石、磷灰石核飛跡年代、鉀長石氩氩年代皆有明顯差異:在拉薩河流域有非常比例的年輕族群,而尼洋河流域並無明顯的年輕年代訊號。由鋯石的核飛跡-鈾鉛雙重定年法結果顯示,年輕的核飛跡年代主要指示在拉薩河流域內有強烈的剝蝕事件發生。藉由上游與下游沉積物氩氩年代的對比,我們確認了主要的沉積物來源應為拉薩河流域中跨過念青唐古拉山脈前緣(即古露張裂帶谷地)的區域。 | zh_TW |
dc.description.abstract | Tibetan plateau is one of the most phenomenal orogens in the world. The spectacular landscape provides the opportunity to understand the fundamental mechanisms of mountain building process from varied disciplines such as geomorphology, geochemistry, and geophysics. Like many other orogenic belts around the world, the expedition into the plateau can be hampered by the inaccessibility of intended outcrops. These rough terrains, however, are often the most crucial outcrops to reveal the tectonic picture of the regime. Alternatively, sediments collected from the downstream of selected watershed can reflect a synthetic picture and provide integrated information in a catchment scale. With appropriate strategies and targets, we can therefore establish a comprehensive understanding toward the aimed tributaries and distinguish the veiled governing forces.
In this study, we used multiple thermo-chronometers to detect the provenance of modern sediments from two tributaries of Yarlung-Tsangpo River, southeast Tibet. Results from zircon fission track (ZFT), apatite fissiontrack (AFT), Ar-Ar single grain analysis on K-feldspar and U/Pb-ZFT double dating all indicate the occurrence of grains with young thermal ages prevailing in the Lhasa River. This remarkable young population is not significantly detected in the Nyang River, another tributary east of Lhasa River. The discrepancy of age population between the two catchments suggests that the fundamental surface process must be different. Zircon U/Pb and fission track double dating suggests that the young age component represent the recent exhumation episode in Lhasa River. Comparisons between downstream, upstream sediments and in situ rock samples inside Lhasa River explicate that the provenance of the young grains is related to the major structure, Gulu Rifting belt. The high percentage of these young grains suggests a focused denudation in a restricted area of the Lhasa River, mostly along the Nyainqentanglha range. | en |
dc.description.provenance | Made available in DSpace on 2021-06-08T01:10:42Z (GMT). No. of bitstreams: 1 ntu-103-D94224003-1.pdf: 13361990 bytes, checksum: f7e11d42bcaf8f91489836b086a07357 (MD5) Previous issue date: 2014 | en |
dc.description.tableofcontents | 口試委員審定書 i
謝辭 ii 中文摘要 iii Abstract iv Highlights vi List of figures ix List of tables x Chapter 1. Introduction 1 1.1 Geological background of Tibet 3 1.2 Detrital study and multiple thermo-chronometers 4 Chapter 2. Sampling strategy and analytical methods 8 2.1 Study area 8 2.2 Analytical methods 11 2.2.1 Fission track dating 14 2.2.1.1 Principles of fission track dating 14 2.2.1.2 Purpose and limit 15 2.2.1.3 Operation procedures 16 2.2.2 Ar-Ar dating 17 2.2.2.1 Principles of Ar-Ar dating 17 2.2.2.2 Purpose and limit 17 2.2.2.3 Operation procedures 17 2.2.3 LA-ICPMS Zircon U/Pb dating 19 2.2.3.1 Principles of U/Pb dating 19 2.2.3.2 Purpose and limit 19 2.2.3.3 Operation procedure 20 Chapter 3. Results 22 3.1 Zircon fission track results 22 3.1.1 ZFT results of sample LS 23 3.1.2 ZFT results of sample SR 24 3.1.3 ZFT results of sample BY 25 3.2 Apatite fission track 26 3.3 Ar-Ar 27 3.4 U/Pb 29 Chapter 4. Discussions 30 4.1 Discrepancy of age population between Lhasa and Nyang Rivers 30 4.1.1 ZFT 31 4.1.2 Ar-Ar 34 4.1.3 AFT 36 4.1.4 Young age components prevail in Lhasa River 37 4.2 What do the young thermo ages represent? 38 4.2.1 Zircon double dating of LS 40 4.2.2 Zircon double dating of BY 41 4.2.3 Comparisons of double datings between Lhasa and Nyang River 42 4.3 Where are the young grains from? 44 4.3.1 Hypsometry of the two tributaries 44 4.3.2 Tracking the provenance 47 Chapter 5. Conclusions 52 References 54 Appendix I. Detailed results of Ar-Ar analyses 59 Appendix II. Detailed results of U/Pb analyses 73 Appendix III.1. LS Zircon fission track results 83 Appendix III.2. SR Zircon fission track results 96 Appendix III.3. BY Zircon fission track results 107 Appendix IV.1. Publications I 113 Appendix IV.2. Publications II 127 | |
dc.language.iso | en | |
dc.title | 運用多重熱定年法探討雅魯藏布江支流之碎屑物源 | zh_TW |
dc.title | Provenance tracking deduced by multiple thermochronometers on detrital minerals from the Yarlung-Tsangpo, southeast Tibet | en |
dc.type | Thesis | |
dc.date.schoolyear | 102-2 | |
dc.description.degree | 博士 | |
dc.contributor.oralexamcommittee | 劉聰桂,羅清華,藍晶瑩,李元希,鍾孫霖 | |
dc.subject.keyword | 核飛跡定年,氬氬定年,鈾鉛定年,熱定年,源區研究,古露張裂帶, | zh_TW |
dc.subject.keyword | Fission track dating,Ar-Ar dating,U/Pb dating,Thermo-chronology,Provenance study,Gulu Rifting belt, | en |
dc.relation.page | 138 | |
dc.rights.note | 未授權 | |
dc.date.accepted | 2014-08-17 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 地質科學研究所 | zh_TW |
顯示於系所單位: | 地質科學系 |
文件中的檔案:
檔案 | 大小 | 格式 | |
---|---|---|---|
ntu-103-1.pdf 目前未授權公開取用 | 13.05 MB | Adobe PDF |
系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。