請用此 Handle URI 來引用此文件：
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/60598完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 沈川洲(Chuan-Chou Shen),施路易(Ludvig Lowemark) | |
| dc.contributor.author | Hao-Cheng Wang | en |
| dc.contributor.author | 王皓正 | zh_TW |
| dc.date.accessioned | 2021-06-16T10:22:55Z | - |
| dc.date.available | 2015-08-26 | |
| dc.date.copyright | 2013-08-26 | |
| dc.date.issued | 2013 | |
| dc.date.submitted | 2013-08-15 | |
| dc.identifier.citation | Alley, R. B., P. A. Mayewski, T. Sowers, M. Stuiver, K. C. Taylor & P. U. Clark (1997) Holocene climatic instability: A prominent, widespread event 8200 yr ago. Geology, 25, 483-486.
An, Z., T. Liu, Y. Lu, S. C. Porter, G. Kukla, X. Wu & Y. Hua (1990) The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China. Quaternary International, 7–8, 91-95. An, Z. S. (2000) The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews, 19, 171-187. Andersen, K. K., A. Svensson, S. J. Johnsen, S. O. Rasmussen, M. Bigler, R. Rothlisberger, U. Ruth, M. L. Siggaard-Andersen, J. P. Steffensen, D. Dahl-Jensen, B. M. Vinther & H. B. Clausen (2006) The Greenland Ice Core Chronology 2005, 15-42 ka. Part 1: constructing the time scale. Quaternary Science Reviews, 25, 3246-3257. Barber, D. C., A. Dyke, C. Hillaire-Marcel, A. E. Jennings, J. T. Andrews, M. W. Kerwin, G. Bilodeau, R. McNeely, J. Southon, M. D. Morehead & J. M. Gagnon (1999) Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes. Nature, 400, 344-348. Braconnot, P., M. F. Loutre, B. Dong, S. Joussaume, P. Valdes & P. P. Grps (2002) How the simulated change in monsoon at 6 ka BP is related to the simulation of the modern climate: results from the Paleoclimate Modeling Intercomparison Project. Climate Dynamics, 19, 107-121. Broccoli, A. J., K. A. Dahl & R. J. Stouffer (2006) Response of the ITCZ to Northern Hemisphere cooling. Geophysical Research Letters, 33. Burns, S. J., D. Fleitmann, A. Matter, U. Neff & A. Mangini (2001) Speleothem evidence from Oman for continental pluvial events during interglacial periods. Geology, 29, 623-626. Burns, S. J., A. Matter, N. Frank & A. Mangini (1998) Speleothem-based paleoclimate record from northern Oman. Geology, 26, 499-502. Cheng, H., R. L. Edwards, Y. J. Wan, X. G. Ko, Y. F. Ming, M. J. Kelly, X. F. Wang, C. D. Gallup & W. G. Liu (2006) A penultimate glacial monsoon record from Hulu Cave and two-phase glacial terminations. Geology, 34, 217-220. Cheng, H., R. Lawrence Edwards, C.-C. Shen, V. J. Polyak, Y. Asmerom, J. Woodhead, J. Hellstrom, Y. Wang, X. Kong, C. Spotl, X. Wang & E. Calvin Alexander Jr (2013) Improvements in 230Th dating, 230Th and 234U half-life values, and U–Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry. Earth and Planetary Science Letters, 371–372, 82-91. Cheng, H., A. Sinha, X. F. Wang, F. W. Cruz & R. L. Edwards (2012) The Global Paleomonsoon as seen through speleothem records from Asia and the Americas. Climate Dynamics, 39, 1045-1062. Chiang, J. C. H., M. Biasutti & D. S. Battisti (2003) Sensitivity of the Atlantic Intertropical Convergence Zone to Last Glacial Maximum boundary conditions. Paleoceanography, 18. Chodankar, A. R., V. K. Banakar & T. Oba (2005) Past 100 ky surface salinity-gradient response in the Eastern Arabian Sea to the summer monsoon variation recorded by delta O-18 of G. sacculifer. Global and Planetary Change, 47, 135-142. Claussen, M., C. Kubatzki, V. Brovkin, A. Ganopolski, P. Hoelzmann & H. J. Pachur (1999) Simulation of an abrupt change in Saharan vegetation in the mid-Holocene. Geophysical Research Letters, 26, 2037-2040. Dayem, K. E., P. Molnar, D. S. Battisti & G. H. Roe (2010) Lessons learned from oxygen isotopes in modern precipitation applied to interpretation of speleothem records of paleoclimate from eastern Asia. Earth and Planetary Science Letters, 295, 219-230. deMenocal, P., J. Ortiz, T. Guilderson, J. Adkins, M. Sarnthein, L. Baker & M. Yarusinsky (2000) Abrupt onset and termination of the African Humid Period: rapid climate responses to gradual insolation forcing. Quaternary Science Reviews, 19, 347-361. Desmarchelier, J. M., A. Goede, L. K. Ayliffe, M. T. McCulloch & K. Moriarty (2000) Stable isotope record and its palaeoenvironmental interpretation for a late Middle Pleistocene speleothem from Victoria Fossil Cave, Naracoorte, South Australia. Quaternary Science Reviews, 19, 763-774. Ding, Z. L., N. Rutter, J. T. Han & T. S. Liu (1992) A Coupled Environmental System Formed at About 2.5 Ma in East-Asia. Palaeogeography Palaeoclimatology Palaeoecology, 94, 223-242. Dorale, J. A. & Z. H. Liu (2009) Limitations of Hendy Test Criteria in Judging the Paleoclimatic Suitability of Speleothems and the Need for Replication. Journal of Cave and Karst Studies, 71, 73-80. Duplessy, J. C. (1982) Glacial to Interglacial Contrasts in the Northern Indian-Ocean. Nature, 295, 494-498. Dykoski, C. A., R. L. Edwards, H. Cheng, D. X. Yuan, Y. J. Cai, M. L. Zhang, Y. S. Lin, J. M. Qing, Z. S. An & J. Revenaugh (2005) A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters, 233, 71-86. Fairchild, I. J., C. L. Smith, A. Baker, L. Fuller, C. Spotl, D. Mattey, F. McDermott & Eimp (2006) Modification and preservation of environmental signals in speleothems. Earth-Science Reviews, 75, 105-153. Fleitmann, D., S. J. Burns, A. Mangini, M. Mudelsee, J. Kramers, I. Villa, U. Neff, A. A. Al-Subbary, A. Buettner, D. Hippler & A. Matter (2007) Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen (Socotra). Quaternary Science Reviews, 26, 170-188. Fleitmann, D., S. J. Burns, M. Mudelsee, U. Neff, J. Kramers, A. Mangini & A. Matter (2003) Holocene forcing of the Indian monsoon recorded in a stalagmite from Southern Oman. Science, 300, 1737-1739. Fleitmann, D., S. J. Burns, M. Pekala, A. Mangini, A. Al-Subbary, M. Al-Aowah, J. Kramers & A. Matter (2011) Holocene and Pleistocene pluvial periods in Yemen, southern Arabia. Quaternary Science Reviews, 30, 783-787. Frumkin, A., I. Carmi, A. Gopher, D. C. Ford, H. P. Schwarcz & T. Tsuk (1999) A Holocene millennial-scale climatic cycle from a speleothem in Nahal Qanah Cave, Israel. Holocene, 9, 677-682. Gasse, F. (2000) Hydrological changes in the African tropics since the Last Glacial Maximum. Quaternary Science Reviews, 19, 189-211. Gasse, F. & E. Van Campo (1994) Abrupt post-glacial climate events in West Asia and North Africa monsoon domains. Earth and Planetary Science Letters, 126, 435-456. Global Network of Isotope in Precipitation, GIS Global Mapping System for Isotopes in the Water Cycle, International Atomic Energy Agency at http://www.iaea.org/water/ Goede, A., D. C. Green & R. S. Harmon (1986) Late Pleistocene Paleotemperature Record from a Tasmanian Speleothem. Australian Journal of Earth Sciences, 33, 333-342. Gonfiantini, R., M. A. Roche, J. C. Olivry, J. C. Fontes & G. M. Zuppi (2001) The altitude effect on the isotopic composition of tropical rains. Chemical Geology, 181, 147-167. Gupta, A. K., D. M. Anderson & J. T. Overpeck (2003) Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature, 421, 354-357. Harmon, R. S., P. Thompson, H. P. Schwarcz & D. C. Ford (1978) Late Pleistocene Paleoclimates of North-America as Inferred from Stable Isotope Studies of Speleotherms. Quaternary Research, 9, 54-70. Hendy, C. H. (1971) Isotopic Geochemistry of Speleothems .1. Calculation of Effects of Different Modes of Formation on Isotopic Composition of Speleothems and Their Applicability as Palaeoclimatic Indicators. Geochimica Et Cosmochimica Acta, 35, 801-824. Hutson, W. H. & W. L. Prell (1980) Paleoecological Transfer-Function, Fi-2, for Indian-Ocean Planktonic-Foraminifera. Journal of Paleontology, 54, 381-399. Ivanochko, T. S., R. S. Ganeshram, G. J. A. Brummer, G. Ganssen, S. J. A. Jung, S. G. Moreton & D. Kroon (2005) Variations in tropical convection as an amplifier of global climate change at the millennial scale. Earth and Planetary Science Letters, 235, 302-314. Kim, S. T. & J. R. Oneil (1997) Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates. Geochimica Et Cosmochimica Acta, 61, 3461-3475. Kutzbach, J. E. & Z. Liu (1997) Response of the African monsoon to orbital forcing and ocean feedbacks in the middle Holocene. Science, 278, 440-443. Lachniet, M. S. (2009) Climatic and environmental controls on speleothem oxygen-isotope values. Quaternary Science Reviews, 28, 412-432. Lazareth, C. E., M. G. B. Rosell, B. Turcq, F. Le Cornec, M. Mandeng-Yogo, S. Caquineau & G. Cabioch (2013) Mid-Holocene climate in New Caledonia (southwest Pacific): coral and PMIP models monthly resolved results. Quaternary Science Reviews, 69, 83-97. Lezine, A. M., C. Robert, S. Cleuziou, M. L. Inizan, F. Braemer, J. F. Saliege, F. Sylvestre, J. J. Tiercelin, R. Crassard, S. Mery, V. Charpentier & T. Steimer-Herbet (2010) Climate change and human occupation in the Southern Arabian lowlands during the last deglaciation and the Holocene. Global and Planetary Change, 72, 412-428. North Greenland Ice Core Project members, 2004 O'Neil, J. R. & H. P. Taylor (1969) Oxygen isotope equilibrium between muscovite and water. Journal of Geophysical Research, 74, 6012-6022. Parker, A. G., A. S. Goudie, S. Stokes, K. White, M. J. Hodson, M. Manning & D. Kennet (2006) A record of Holocene climate change from lake geochemical analyses in southeastern Arabia. Quaternary Research, 66, 465-476. Partin, J. W., K. M. Cobb, J. F. Adkins, B. Clark & D. P. Fernandez (2007) Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum. Nature, 449, 452-455. Pausata, F. S. R., D. S. Battisti, K. H. Nisancioglu & C. M. Bitz (2011) Chinese stalagmite delta O-18 controlled by changes in the Indian monsoon during a simulated Heinrich event. Nature Geoscience, 4, 474-480. Porter, S. C. & Z. S. An (1995) Correlation between Climate Events in the North-Atlantic and China during Last Glaciation. Nature, 375, 305-308. Porter, S. C., Z. S. An & H. B. Zheng (1992) Cyclic Quaternary Alluviation and Terracing in a Nonglaciated Drainage-Basin on the North Flank of the Qinling Shan, Central China. Quaternary Research, 38, 157-169. Prell, W. L., W. H. Hutson, D. F. Williams, A. W. H. Be, K. Geitzenauer & B. Molfino (1980) Surface Circulation of the Indian-Ocean during the Last Glacial Maximum, Approximately 18,000 Yr Bp. Quaternary Research, 14, 309-336. Radies, D., S. T. Hasiots, F. Preusser, E. Neubert & A. Matter (2005) Paleoclimatic significance of Early Holocene faunal assemblages in wet interdune deposits of the Wahiba Sand Sea, sultanate of Oman. Journal of Arid Environments, 62, 109-125. Rashid, H., E. England, L. Thompson & L. Polyak (2011) Late Glacial to Holocene Indian Summer Monsoon Variability Based upon Sediment Records Taken from the Bay of Bengal. Terrestrial Atmospheric and Oceanic Sciences, 22, 215-228. Rashid, H., B. P. Flower, R. Z. Poore & T. M. Quinn (2007) A similar to 25 ka Indian Ocean monsoon variability record from the Andaman Sea. Quaternary Science Reviews, 26, 2586-2597. Rasmussen, S. O., K. K. Andersen, A. M. Svensson, J. P. Steffensen, B. M. Vinther, H. B. Clausen, M. L. Siggaard-Andersen, S. J. Johnsen, L. B. Larsen, D. Dahl-Jensen, M. Bigler, R. Rothlisberger, H. Fischer, K. Goto-Azuma, M. E. Hansson & U. Ruth (2006) A new Greenland ice core chronology for the last glacial termination. Journal of Geophysical Research-Atmospheres, 111. Saher, M. H., F. J. C. Peeters & D. Kroon (2007) Sea surface temperatures during the SW and NE monsoon seasons in the western Arabian Sea over the past 20,000 years. Palaeogeography Palaeoclimatology Palaeoecology, 249, 216-228. Saraswat, R., Nigam, R., Mackensen, A., & Weldeab, S. (2012) Linkage between seasonal insolation gradient in the tropical northern hemisphere and the sea surface salinity of the equatorial Indian Ocean during the last glacial period. Acta Geologica. Sinica, 86, 801-811. Schrag, D. P., G. Hampt & D. W. Murray (1996) Pore fluid constraints on the temperature and oxygen isotopic composition of the glacial ocean. Science, 272, 1930-1932. Schulz, H., U. von Rad & H. Erlenkeuser (1998) Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years. Nature, 393, 54-57. Shen, C. C., H. Cheng, R. L. Edwards, S. B. Moran, H. N. Edmonds, J. A. Hoff & R. B. Thomas (2003) Measurement of attogram quantities of Pa-231 in dissolved and particulate fractions of seawater by isotope dilution thermal ionization mass spectroscopy. Analytical Chemistry, 75, 1075-1079. Shen, C. C., K. S. Li, K. Sieh, D. Natawidjaja, H. Cheng, X. Wang, R. L. Edwards, D. D. Lam, Y. T. Hsieh, T. Y. Fan, A. J. Meltzner, F. W. Taylor, T. M. Quinn, H. W. Chiang & K. H. Kilbourne (2008) Variation of initial Th-230/Th-232 and limits of high precision U-Th dating of shallow-water corals. Geochimica Et Cosmochimica Acta, 72, 4201-4223. Shen, C. C., C. C. Wu, H. Cheng, R. L. Edwards, Y. T. Hsieh, S. Gallet, C. C. Chang, T. Y. Li, D. D. Lam, A. Kano, M. Hori & C. Spotl (2012) High-precision and high-resolution carbonate Th-230 dating by MC-ICP-MS with SEM protocols. Geochimica Et Cosmochimica Acta, 99, 71-86. Sinha, A., K. G. Cannariato, L. D. Stott, H. C. Li, C. F. You, H. Cheng, R. L. Edwards & I. B. Singh (2005) Variability of Southwest Indian summer monsoon precipitation during the Boiling-Allerod. Geology, 33, 813-816. Sirocko, F., M. Sarnthein, H. Erlenkeuser, H. Lange, M. Arnold & J. C. Duplessy (1993) Century-Scale Events in Monsoonal Climate over the Past 24,000 Years. Nature, 364, 322-324. Sonzogni, C., E. Bard & F. Rostek (1998) Tropical sea-surface temperatures during the last glacial period: A view based on alkenones in Indian Ocean sediments. Quaternary Science Reviews, 17, 1185-1201. Street, F. A. & A. T. Grove (1979) Global Maps of Lake-Level Fluctuations since 30,000 Yr Bp. Quaternary Research, 12, 83-118. Svensson, A., K. K. Andersen, M. Bigler, H. B. Clausen, D. Dahl-Jensen, S. M. Davies, S. J. Johnsen, R. Muscheler, S. O. Rasmussen, R. Rothlisberger, J. P. Steffensen & B. M. Vinther (2006) The Greenland Ice Core Chronology 2005, 15-42 ka. Part 2: comparison to other records. Quaternary Science Reviews, 25, 3258-3267. Thai Meteorological Department at http://www.tmd.go.th/en/ Trenberth, K. E., D. P. Stepaniak & J. M. Caron (2000) The global monsoon as seen through the divergent atmospheric circulation. Journal of Climate, 13, 3969-3993. von Rad, U., H. Schulz, V. Riech, M. den Dulk, U. Berner & F. Sirocko (1999) Multiple monsoon-controlled breakdown of oxygen-minimum conditions during the past 30,000 years documented in laminated sediments off Pakistan. Palaeogeography, Palaeoclimatology, Palaeoecology, 152, 129-161. Waelbroeck, C., L. Labeyrie, E. Michel, J. C. Duplessy, J. F. McManus, K. Lambeck, E. Balbon & M. Labracherie (2002) Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records. Quaternary Science Reviews, 21, 295-305. Wang, B. (2006) The Asian monsoon. Praxis Publishling Ltd. Wang, B. & LinHo (2002) Rainy season of the Asian-Pacific summer monsoon. Journal of Climate, 15, 386-398. Wang, L., M. Sarnthein, H. Erlenkeuser, J. O. Grimalt, P. Grootes, S. Heilig, E. Ivanova, M. Kienast, C. Pelejero & U. Pflaumann (1999) East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the south China Sea. Marine Geology, 156, 245-284. Wang, L. J. & P. X. Wang (1990) Late Quaternary Paleoceanography of the South China Sea: Glacial-Interglacial Contrasts in an Enclosed Basin. Paleoceanography, 5, 77-90. Wang, Y. J., H. Cheng, R. L. Edwards, Z. S. An, J. Y. Wu, C. C. Shen & J. A. Dorale (2001) A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China. Science, 294, 2345-2348. Wang, Y. J., H. Cheng, R. L. Edwards, Y. Q. He, X. G. Kong, Z. S. An, J. Y. Wu, M. J. Kelly, C. A. Dykoski & X. D. Li (2005) The Holocene Asian monsoon: Links to solar changes and North Atlantic climate. Science, 308, 854-857. Wang, Y. J., H. Cheng, R. L. Edwards, X. G. Kong, X. H. Shao, S. T. Chen, J. Y. Wu, X. Y. Jiang, X. F. Wang & Z. S. An (2008) Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature, 451, 1090-1093. Xu, J. A., W. Kuhnt, A. Holbourn, M. Regenberg & N. Andersen (2010) Indo-Pacific Warm Pool variability during the Holocene and Last Glacial Maximum. Paleoceanography, 25. Yancheva, G., N. R. Nowaczyk, J. Mingram, P. Dulski, G. Schettler, J. F. W. Negendank, J. Q. Liu, D. M. Sigman, L. C. Peterson & G. H. Haug (2007) Influence of the intertropical convergence zone on the East Asian monsoon. Nature, 445, 74-77. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/60598 | - |
| dc.description.abstract | 亞洲季風是全球氣候系統的重要系統之一，前人的研究認為亞洲季風不止與北半球高緯度地區變化有關，同時也受到南半球赤道地區變化所影響，前人已經透過中國和印度的氧同位素記錄重建了亞洲季風過去的變化，並顯示此一強度變化主要受控於北半球高緯度地區夏季日照量影響。然而，末次冰期以來洞穴石筍紀錄卻鮮少來自於低緯度地區，因此在亞洲季風演化過程的解釋上可能造成些許不確定。透過七支採集自泰國南部Klang洞穴（8°1'N，98°48'E）的石筍樣本，並利用其氧同位素紀錄，我們重建了過去兩萬三千年以來低緯度地區亞洲季風的變化。此研究結果支持了前人在此時間段的亞洲季風研究成果，包含末次冰期、Heinrich event 1、新仙女木事件（YD）等氣候皆有同步變化的現象。亞洲季風區洞穴石筍氧同位素變化的一致性說明過去亞洲季風的強弱主要跟隨北半球日照量而改變，但Klang洞穴記錄在Termination 1、新仙女木事件（YD）等氣候事件的變化幅度上卻是中國石筍的二到三倍，根據現代降雨觀測及雨水氧同位素值顯示，我們認為此一現象不只與亞洲夏季季風有關，同時也受到亞洲冬季季風的影響。 | zh_TW |
| dc.description.abstract | The Asian monsoon (AM) is an important component of the global climate system. Its past variability, revealed by Chinese and Indian cave carbonate records, was paced by solar forcing and strongly influenced by changes in northern high-latitude climatic condition. However, only a few absolutely dated records are available from low latitude. Here, I present a replicated and spliced stalagmite record covering the past twenty-three thousand years from Klang Cave in southern Thailand (8°1'N, 98°48'E). Synchroneity of climate changes recorded in different Asian caves and in the Greenland oxygen isotope record support previous assumptions of orbital and high-latitudinal forcings. However, the respective enrichment and depletion in δ18O values over the Younger Dryas and Termination 1 of Klang record are 2-3 times greater than those registered in the Chinese cave records. On the basis of modern monthly rainfall data and their oxygen isotopic values, I propose that Klang Cave stalagmite δ18O variability is not only associated with the Asian summer monsoon, but also with the Asian winter monsoon. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-16T10:22:55Z (GMT). No. of bitstreams: 1 ntu-102-R00224103-1.pdf: 6671231 bytes, checksum: 44ce1d6deac0c08f17073900cc5676a9 (MD5) Previous issue date: 2013 | en |
| dc.description.tableofcontents | 誌謝 I
Abstract II 摘要 III Content IV List of Figures VI List of Tables VIII Chapter 1 Introduction 1 1.1 Asian monsoon 1 1.2 Asian paleomonsoon 3 1.3 Cave system δ18O as paleoclimate proxy 4 Chapter 2 Regional setting 6 2.1 Location 6 2.2 Climate 7 Chapter 3 Material and methods 9 3.1 Material 9 3.2 230Th dating 12 3.3 Stable isotope 13 Chapter 4 Results 15 4.1 230Th dating data 15 4.2 Replication 26 4.3 Oxygen isotopes profile 28 Chapter 5 Discussion 30 5.1 δ18O variation of Klang cave stalagmites 30 5.2 From LGM to YD 35 5.3 The Holocene 39 Chapter 6 Conclusions 45 Reference 46 Appendix I Chemical procedure 61 Appendix II Uranium and thorium isotopic concentration data 65 Appendix III Oxygen isotope records 70 | |
| dc.language.iso | en | |
| dc.subject | 石筍 | zh_TW |
| dc.subject | 亞洲季風 | zh_TW |
| dc.subject | stalagmite | en |
| dc.subject | Asian monsoon | en |
| dc.title | 由泰國Klang洞穴石筍紀錄探討過去兩萬三千年以來亞洲季風變化 | zh_TW |
| dc.title | Asian monsoon variability over the past 23,000 years recorded in stalagmites from Klang Cave, Thailand | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 101-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 魏國彥,米泓生,李時雨 | |
| dc.subject.keyword | 石筍,亞洲季風, | zh_TW |
| dc.subject.keyword | stalagmite,Asian monsoon, | en |
| dc.relation.page | 98 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2013-08-16 | |
| 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-102-1.pdf 未授權公開取用 | 6.51 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。