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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
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dc.contributor.advisor | 楊燦堯 | |
dc.contributor.author | Ling Chung | en |
dc.contributor.author | 鍾靈 | zh_TW |
dc.date.accessioned | 2021-06-13T04:16:31Z | - |
dc.date.available | 2006-07-27 | |
dc.date.copyright | 2006-07-27 | |
dc.date.issued | 2006 | |
dc.date.submitted | 2006-07-24 | |
dc.identifier.citation | 許瑞芳(2000)雲南高黎貢山剪切帶之熱定年學研究。國立台灣大學地質學研究所碩士論文,共86頁。
楊逸籌、李炳元、尹澤生、張青松、王富葆、景可與陳志明(1983)西藏地貌-青藏高原科學考察叢書,科學出版社,共238頁。 潘裕生與孔祥儒(1998)青藏高原岩石圈結構演化和動力學。廣東科技出版社,共428頁。 Amano, K. and Taira, A. (1992) Two-phase uplift of Higher Himalayas since 17 Ma. Geology, 20, 391-394. Armijo, R., Tapponnier, P. and Han, T.L. (1989) Late Cenozoic right-lateral faulting in southern Tibet. J. Geophys. Res., 94, 2787-2838. Baard, J.H., Zijp, W.L. and Nolthenius, H.J. (1989) Nuclear data guide for reactor metrology. Kluwer Acad. Publ., 372 pp. Bertrand, G., Ragin, C., Maluski, H., Tin, A.H., Myint, T., Ohn, M., Win, M. and San, L. (1999) Cenozoic metamorphism along the Shan scarp (Myanmar): evidence for ductile shear along the Sagaing fault or the northward migration of the eastern Himalayan Syntaxis. Geophys. Res. Lett., 26, 915-918. Brandon, M.T. (1992) Decomposition of fission-track grain-age distributions. Am. J. Sci., 292, 535-564. Brandon, M.T. (1996) Probability density plot for fission-track grain-age samples. Radiat. Meas., 26, 663-676. Brandon, M.T. and Vance, J.A. (1992) Tectonic evolution of the Cenozoic Olympic subduction complex, Washington State, as deduced from fission track ages for detrital zircons. Am. J. Sci., 292, 565-636. Burg, J.P., Nievergelt, P., Oberli, F., Seward, D., Davy, P., Maurin, J.C., Diao, Z. and Meier, M. (1998) The Namche Barwa syntaxis: evidence for exhumation related ot compressional crustal folding. J. Asian Earth Sci., 16, 239-252. Cande, S.C. and Kent, D.V. (1992) A new geomagnetic polarity time scale for the Late Cretaceous and Cenozoic. J. Geophys. Res., 97, 13,917-13,951. Cande, S.C. and Kent D.V. (1995) Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic. J. Geophys. Res., 100, 6093-6095. Carter, A. and Moss, S.J. (1999) Combined detrital-zircon fission-track and U-Pb dating: A new approach to understanding hinterland evolution. Geology, 27, 235-238 Chen, Z., Burchfiel, B.C., Liu, Y., King, R.W., Royden, L.H., Tang, W., Wang, E., Zhao, J. and Zhang, X. (2000) Global position system measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation. J. Geophys. Res., 105, 16,215-16,227. Chung, S.L., Chu, M.F., Zhang, Y., Xie, Y., Lo, C.H., Lee, T.Y., Lan, C.Y., Li, X., Zhang, Q. and Wang, Y. (2005) Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism. Earth-Sci. Rev., 68, 173-196. Chung, S.L., Lee, T.Y., Lo, C.H., Wang, P.L., Chen, C.Y., Nguyen, T.Y., Tran, T.H. and Wu, G.Y. (1997) Intraplate extension prior to continental extrusion along the Ailao Shan-Red River shear zone. Geology, 25, 311-314. Chung, S.L., Lo, C.H., Lee, T.Y., Zhang, Y., Xie, Y., Li, X., Wang, K.L. and Wang, P.L. (1998) Diachronous uplift of the Tibetan plateau staring 40 Myr ago. Nature, 394, 769-773. Clark, M.K., House, M.A., Royden, L.H., Whipple, K.X., Burchfiel, B.C., Zhang, X. and Tang, W. (2005) Late Cenozoic uplift of southeastern Tibet. Geology, 33, 525-528. Clark, M.K., Schoenbohm, L.M., Royden, L.H., Whipple, K.X., Burchfiel, B.C., Zhang, X., Tang, W., Wang, E. and Chen, L. (2004) Surface uplift, tectonics, and erosion of eastern Tibet from large-scale drainage patterns. Tectonics, 23, TC1006, doi:10.1029/2002TC001402. Ding, L., Zhong, D., Yin, A., Kapp, P. and Harrison, T.M. (2001) Cenozoic structural and metamorphic evolution of the eastern Himalayan syntaxis (Namche Barwa). Earth Planet. Sci. Lett., 192, 423-438. Dunlap, W.J., Weinberg, R.F. and Searle, M.P. (1998) Karakoram fault zone rocks cool in two phases. J. Geol. Soc. London, 155, 903-912. England, P.C. and Houseman, G.A. (1989) Extension during continental convergence, with application to the Tibetan Plateau. J. Geophys. Res., 94, 17,561-17,579. Farley, K.A. (2000) Helium diffusion from apatite: General behavior as illustrated by Durango fluorapatite. J. Geophys. Res., 105, 2903-2914. Fleicher, R.L. and Price, P.B. (1964) Decay constant for spontaneous fission of 238U. Phys. Rev., 133B, 63-64. Fleicher, R.L., Price, P.B. and Walker, R.M. (1965) The ion explosion spike mechanism of formation of charged particle tracks in solids. J. Appl. Phys., 36, 3645-3652. Galbraith, R.F. (1988) Graphical display of estimates having differing standard errors. Tectonometrics, 30, 271-281. Gallagher, K., Brown, R. and Johnson, C. (1998) Fission track analysis and its applications to geological problems. Ann. Rev. Earth Planet. Sci., 26, 519-572. Garver, J.I., Brandon, M.T., Roden-Tice, M.K. and Kamp, P.J.J. (1999) Exhumation history of orogenic highlands determined by detrital fission track thermochronology. In: Ring, U., Brandon, M.T., Willett, S.D., Lister, D.S. (Eds.) Exhumation processes: Normal faulting, ductile flow, and erosion. Geol. Soc. London Sp. Pub., 154, 283-304. Garzanti, E., Vezzoli, G., Ando, S., Christian, F.L., Singh, S.K. and Foster, G. (2004) Sand petrology and focused erosion in collision orogens: The Brahmaputra case. Earth Planet. Sci. Lett., 220, 157-174. Haack, U. (1977) The closing temperature for fission track retention in minerals. Am. J. Sci., 277, 459-464. Hallet, B. and Molnar, P. (2001) Distorted drainage basins as markers of crustal strain east of the Himalaya. J. Geophys. Res., 106, 13,697-13,709. Harrison, T.M., Copeland, P., Kidd, W.S.F. and Yin, A. (1992) Raising Tibet. Science, 255, 1633-1670. Holden, N.E. (1989) Total and spontaneous fission half-lives for uranium, plutonium, americium and curium nuclides. Pure Appl. Chem., 61, 1483-1504. Houseman, G.A., Mckenzie, D.P. and Molnar, P.J. (1981) Convective instability of a thickened boundary layer and its relevance for the thermal evolution of continental convergent belts. J. Geophys. Res., 86, 6115-6132. Hurfold, A.J. (1986) Cooling and Uplift patterns in the Lepontine Alps South Central Switzerland and an age of vertical movement on the Insubric fault line. Contrib. Miner. Petrol., 92, 413-427. Hurfold, A.J. and Green, P.F. (1983) The Zeta age calibration of fission track dating. Isot. Geosci., 1, 285-317. James, K. and Durrani, S.A. (1986) The effect of crystal composition on fission-track annealing and closure temperature in geological minerals: Implication for the cooling rates of the terrestrial and extraterrestrial rocks. Nucl. Tracks Radiat. Meas., 11, 277-282. Kirby, E., Reiners, P.W., Krol, M.A., Whipple, K.X., Hodges, K.V., Farley, K.A., Tang, W. and Chen, Z. (2002) Late Cenozoic evolution of the eastern margin of the Tibetan Plateau: Inferences from 40Ar/39Ar and (U-Th)/He thermochronology. Tectonics, 21, No.1, 1001, 10.1029/2000TC001246. Lacassin, R., Valli, F., Nrnaud, N., Leloup, P.H., Li, H., Tapponnier, P., Paquette, J.L., Chevalier, M.L., Guillot, S. and Xu, Z. (2003) Large-scale geometry and evolution of the Karakorum fault, W-Tibet. Geophys. Res. Abs., 5, 04105. Lee, H.Y., Chung, S.L., Wang, J.R., Wen, D.J., Lo, C.H., Yang, T.F., Zhang, Y.Q., Xie, Y.W., Lee, T.Y., Wu, G.Y. and Ji, J.Q. (2003) Miocene Jiali faulting and its implications for Tibetan tectonic evolution. Earth Planet. Sci. Lett., 205, 185-194. Lee, T.Y., Lo, C.H., Chung, S.L., Chen, C.Y., Wang, P.L., Lin, W.P., Hoang, N., Chi, C.T. and Yem, N.T. (1998) 40Ar/39Ar dating result of Neogene basalts in Vietnam and its tectonic implication. In: J.M.F., Folwer, Chung, S.L., Lo, C.H., Lee, T.Y. (Eds.) Mantle Dynamics and Plate Interaction in East Asia. Am. Geophys. Union Geodynamic Series, 27, 317-330. Leloup, P.H., Lacassin, R., Tapponnier, P., Zhong, D., Liu, X., Zhang, L., Ji, S. and Trinh, P.T. (1995) The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina. Tectonophys., 251, 3-48. Liang, Y.H., Chung, S.L., Liu, D.Y., Xu, Y.G., Wu, F.Y., Yang, J.H., Wang, Y.B. and Lo, C.H. (2006) Detrital zircon evidence from Burma for reorganization of the eastern Himalayan river system. (in prep.) Lin, T.H., Lo, C.H., Chung, S.L., Lee, T.Y., Lee, H.Y. and Hsu, F.J. (2005) New geochronological constraints on the movement of Jiali and Gaoligong shear zones in SE Tibet, and its tectonic implication. Abstract for the 2005 AGU Fall Meeting. San Francisco, USA. Liu, T.K., Chen, Y.G., Chen, W.S. and Jiang, S.H. (2000) Rates of cooling and denudation of the early Penglai orogeny, Taiwan, as assessed by fission-track constraints. Tectonophys., 320, 69-82. Liu, T.K., Hseih, 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 Planet. Sci. Lett., 186, 45-56. McDougall, I. and Harrison, T.M. (1999) Geochronology and thermochronology by the 40Ar/39Ar method. Oxford University Press, Oxford. 269 pp. Molnar, P. and Deng, Q. (1984) Faulting associated with large earthquakes and the average rate of deformation in central and eastern Asia. J. Geophys. Res., 89, 6203-6227. Naeser, C.W. (1979) Fission-track dating and geological annealing of fission tracks. In: Jäger, E. and Hunziker, J.C. (eds.) Lectures in Isotope Geology, Springer-Verlag, 134-169. Nelson, E.P. (1982) Post-tectonic uplift of the Cordillera Darwin orogenic core complex: evidence from fission track geochronology and closing temperature-time relationships. J. Geol. Soc. London, 139, 755-761. Platt, J.P. and England, P.C. (1993) Convective removal of lithosphere beneath mountain belts; thermal and mechanical consequences. Am. J. Sci., 293, 307-336. Price, P.B. and Walker, R.M. (1962) Observations of charged-particle tracks in solids. J. Appl. Phys., 33, 3400-3406. Reiners, P.W., Farley, K.A. and Hickes, H.J. (2002) He diffusion and (U-Th)/He thermochronometry of zircon: Initial results from Fish Canyon Tuff and Gold Butte, Nevada. Tectonophys., 349, 297-308. Roger, F., Callassou, S., Lancelot, J., Malavieille, M., Xu, Z.Q., Hao, Z.W. and Hou, L.W. (1995) Miocene emplacement and deformation of the Konga Shan granite (Xianshui He fault zone, west Sichuan, China): Geodynamic implications. Earth Planet. Sci. Lett., 130, 201-216. Saini, H.S., Sharma, O.P., Parshad, R. and Nagpaul, K.K. (1978) Fission track annealing characteristics of epidote: applications to geochronology and geology. Nuclear Track Detection. Pergamon Press, Oxford-New York. 2, No. 3, 133-139. Sato, K., Liu, Y.Y., Zhu, Z.C., Yang, Z.Y. and Otofuji, Y.I. (1999) Paleomagnetic study of middle Cretaceous rocks from Yunlong, western Yunnan, China: evidence of southward displacement of Indochina. Earth Planet. Sci. Lett., 165, 1-15. Searle, M.P., Weinberg, R.F. and Dunlap, W.J. (1998) Transpressional tectonics along the Karakorum fault zone, northern Ladakh: constraints on Tibetan extrusion. In: R.E. Holdsworth, R.E. Strachan, J.F. Deway (Eds.), Continental Transpressional and Transtensional Tectonics. Geol. Soc. Sp. Pub., 135, 307-326. Spiegel, C., Kuhlemann, J., Dunkl, I., Frisch, W., von Eynatten, H. and Balogh, K. (2000) The history of the Central Alps: Evidence from zircon fission-track data of the foreland basin sediments. Terra Nova, 12, 163-170. Steiger, R.H., and Jäger, E. (1977) Subcommission on geochronology: convention on the use of decay constants in geo- and cosmochronology. Earth Planet. Sci. Lett., 36, 359-362. Tapponnier, P., Peltzer, G., LeDain, A.Y., Armijo, R. and Cobbold, P. (1982) Propagation extrusion tectonics in Asia: New insights from simple experiments with plasticine. Geology, 10, 611-616. Taylor, B. and Hayes, D.E. (1983) Origin and history of the South China Sea Basin. In: D. E. Hayes (Ed.) The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, Part 2, 23-56. Wagner, G.A., Reimen, G.M. and Jager, E. (1977) Cooling ages derived by apatite fission-track, mica Rb-Sr, and K-Ar Dating: The uplift and cooling history of the Central Alps. Padava, Societa Cooperative Topografica, 25p. Wang, P.L., Lo, C.H., Chung, S.L., Lee, T.Y., Lan, C.Y. and Thang, T.V. (2000) Onset timing of left-lateral movement along the Ailao Shan-Red River Shear Zone: 40Ar/39Ar dating constraint from the Nam Dinh Area, northeastern Vietnam. J. Asian Earth Sci., 18, 281-292. Wang, P.L., Lo, C.H., Lee, T.Y., Chung, S.L., Lan, C.Y. and Nguyen, T.Y. (1998) Thermochronological evidence for movement of the Ailao Shan-Red River shear zone: A Vietnamese perspective. Geology, 26, 887-890. Xu, G. and Kamp, P.J.J. (2000) Tectonics and denudation adjacent to the Xianshuihe Fault, eastern Tibetan Plateau: constraints from fission track thermochronology. J. Geophys. Res., 105, 19,231-19,251. Yang, T.F., Wang, J.R., Lo, C.H., Chung, S.L., Tien, J.L., Xu, R. and Deng, W.M. (1999) The thermal history of the Lhasa Block, South Tibetan Plateau based on FTD and Ar-Ar dating. Radiat. Meas., 31, 627-632. Zaun, P.E. and Wagner, G.A. (1985) Fission-track stability in zircons under geological conditions. Nucl. Tracks, 10, No. 3, 303-307 | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/32826 | - |
dc.description.abstract | 喀拉崑崙-嘉黎斷裂帶是由數個右移的錯動帶所組成的巨大斷裂帶,也是向東脫逸之北部青藏高原塊體的南界。嘉黎斷層位於此東西橫貫斷裂帶的最東端,並且是新生代以來構造活動劇烈的東喜馬拉雅山結的北界,其活動不只與向東脫逸的青藏高原塊體有關,更與至今構造活動仍強烈的南迦巴瓦山結息息相關。嘉黎斷裂帶經過通麥後分成兩個分支斷層,帕隆以及布曲斷裂帶,向東南方發育通過察隅地區。本研究地點位於南迦巴瓦山結北方的通麥地區以及東南方的察隅地區。樣本則是採集於斷裂帶中變形或是未變形的岩體,利用核飛跡定年法的分析,以探討藏東地區嘉黎斷裂帶的活動歷史與熱歷史。
分析結果顯示察隅地區之帕隆斷裂帶樣本的鋯石與磷灰石核飛跡年代範圍為ca. 23-19 Ma;布曲斷裂帶之鋯石結果為ca. 10-9 Ma,磷灰石為ca. 6 Ma;通麥地區的定年結果較察隅地區年輕許多,鋯石與磷灰石核飛跡年代皆小於3 Ma。 根據本研究之核飛跡定年數據,嘉黎斷裂帶自開始活動以來,主要活動帶有向南轉移的趨勢。約23-19 Ma時嘉黎斷裂帶的北分支帕隆斷裂帶有一次快速抬升的時期,此次的抬升應與整個嘉黎斷裂帶與其兩分支斷層的錯移有關;18 Ma之後帕隆斷裂帶的活動減緩,印度板塊擠壓的能量轉由藏北塊體順時鐘旋轉所吸收,此時期活動斷層剩下嘉黎-布曲斷層並持續活動至∼11 Ma。本研究於察隅以及通麥地區10 Ma以來不同的核飛跡記錄顯示10-6 Ma應為一次大規模的抬升,影響區域可能廣及整個喜馬拉雅山及西藏東部的許多地區;而3 Ma左右在通麥發生的快速抬升事件(∼2.6 mm/yr)應為區域性事件,導因於印度板塊在東喜馬拉雅山結集中的嵌入式擠壓歐亞大陸板塊,活化了北方的嘉黎斷裂帶所致。察隅與通麥地區異時的抬升順序可能進一步暗示了藏東河川的襲奪順序。 | zh_TW |
dc.description.abstract | Jiali Fault in eastern Tibet bounds the Karakorum-Jiali Fault Zone (KJFZ) in the east and cuts the Namche Barwa Syntaxis northerly. Its movement is not only closely related to the clockwise rotation and extruded body of eastern Tibet, but also strongly correlated to the northeastward indentation of India plate. Representative samples have been collected for fission-track (FT) dating from Jiali fault zone (Tungmai, north of Namche Barwa Syntaxis) and its two easternmost branches, the Parlung and Puqu Faults (near Chayu).
FT ages are analyzed using external detector method. In Chayu region, zircon and apatite FT ages from undeformed granites in Parlung Fault are ca. 23-19 Ma; in the southern branch, Puqu Fault, zircon and apatite FT ages (from both deformed and undeformed rocks) are 10-9 Ma and ca. 6 Ma respectively. In Tungmai area, FT results yield younger ranges than Chayu area (both zircon and apatite ages < 3 Ma from deformed samples). Based on the FT dates in this study, we can conclude that the stress/strain of Jiali Shearing Zone may have shifted from northern branch to southern branch since its initial movement. During 23-19 Ma, the northern branch, Parlung Fault, had undergone an uplifting event which is considered to be related to the shearing of the fault. Consequently, the shearing stress may transfer to the southern branch and had lasted until ~11 Ma. The different ages younger than ~10 Ma obtained from Chayu and Tungmai suggest that the 10-6 Ma uplifting was a large scale event that occurred in Himalayas region and eastern Tibet. However, the uplifting after 3 Ma is believed to be a regional event that resulted from the indentation of India into Eurasia Plate and focusing erosion in Eastern Himalaya Syntaxis. Moreover, the diachronous uplifting in eastern Tibet might provide possible time series constraint for the river capture hypothesis of the unusual drainage system in eastern Tibet. | en |
dc.description.provenance | Made available in DSpace on 2021-06-13T04:16:31Z (GMT). No. of bitstreams: 1 ntu-95-R93224107-1.pdf: 4706029 bytes, checksum: 8afbbb2bcb04176343cf73d5159d2c4a (MD5) Previous issue date: 2006 | en |
dc.description.tableofcontents | 第一章 緒論…………………………………………………………..............1
1.1 研究動機與目的………………………………………………………1 1.2研究區域地質背景與前人工作回顧.....................................................1 第二章 研究原理與方法.................................................................................. 6 2.1核飛跡定年法(Fission Track Dating, FTD)......................................6 2.1.1 核飛跡的生成................................................................................6 2.1.2核飛跡的癒合機制.........................................................................8 2.2核飛跡年代之計算..................................................................................9 2.2.1核飛跡年代之計算公式................................................................10 2.2.2中子通量的計算............................................................................11 2.2.3標準玻璃的ζ(zeta)值...............................................................12 2.2.4年代誤差之計算............................................................................13 2.3核飛跡年代的應用................................................................................14 2.4實驗過程................................................................................................16 2.4.1鋯石礦物樣本的實驗步驟............................................................16 2.4.2磷灰石礦物樣本的實驗步驟........................................................17 2.5核飛跡年代的測定方式........................................................................18 第三章 標本採樣位置與核飛跡定年分析結果.............................................19 3.1標本採集位置........................................................................................19 3.2核飛跡定年分析結果............................................................................21 3.2.1察隅地區........................................................................................22 3.2.1.1 察隅河上游地區................................................................22 3.2.1.2 察隅河中游地區................................................................25 3.2.2通麥地區.......................................................................................28 第四章 綜合討論.............................................................................................31 4.1察隅地區嘉黎帕隆與布曲斷層之異時活動........................................31 4.2通麥與察隅地區中新世以來相異的熱歷史演化................................35 4.3西藏東部自中新世以來之抬升歷史....................................................38 4.4地表抬升對於河流溯源襲奪影響之討論............................................42 第五章 結論.....................................................................................................46 參考文獻...........................................................................................................47 附錄一 核飛跡定年分析數據.........................................................................54 | |
dc.language.iso | zh-TW | |
dc.title | 西藏東部嘉黎斷裂帶熱歷史之核飛跡定年證據及其大地構造之隱示 | zh_TW |
dc.title | Fission Track Ages as Evidence for the Thermal History of Jiala Fault (Eastern Tibet) and its Tectonic Implications | en |
dc.type | Thesis | |
dc.date.schoolyear | 94-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 劉聰桂,陳正宏,藍晶瑩,高銘鴻 | |
dc.subject.keyword | 西藏,嘉黎斷裂帶,核飛跡定年, | zh_TW |
dc.subject.keyword | Tibet,Jiali Fault,Fission track dating, | en |
dc.relation.page | 71 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2006-07-25 | |
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 |
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