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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 楊燦堯 | |
| dc.contributor.author | Chen-Chneg Wang | en |
| dc.contributor.author | 王振丞 | zh_TW |
| dc.date.accessioned | 2021-06-13T08:17:33Z | - |
| dc.date.available | 2005-07-21 | |
| dc.date.copyright | 2005-07-21 | |
| dc.date.issued | 2005 | |
| dc.date.submitted | 2005-07-19 | |
| dc.identifier.citation | 王文祥，1989。大屯火山群之火山學及核飛跡定年： 國立台灣大學地質學研究所碩士論文，共154頁。
何孝恆，2001。台灣北部地區大屯火山群火山噴氣來源之探討：國立台灣大學地質研究所碩士論文，共80頁。 宋聖榮，1989。台灣東部海岸山脈中段火山岩研究兼論北呂宋島弧的演變：國立台灣大學地質學研究所博士論文，共251頁。 李寄嵎，1994。澎湖地區玄武岩類與福建地區基性岩脈之定年學與地球化學研究兼論中生代晚期以來中國東南地函之演化：國立台灣大學地質學研究所博士論文，共226頁。 林蔚，2001。華南沿海地區晚燕山期侵入岩漿活動及大地構造意義。國立台灣大學海洋研究所博士論文，共237頁。 莊文星，1988。台灣新生代晚期火山岩之定年與地球化學研究：國立台灣大學海洋研究所博士論文，共231頁。 莊文星、陳汝勤，1989a。台灣北部火山岩之定年與地球化學研究：經濟部中央地質調查所彙刊，第五號：31-66頁。 莊文星、陳汝勤，1989b。綠島安山岩內之堇青石之探討： 經濟部中央地質調查所彙刊，第五號，67-80頁。 莊文星，1992。台灣之火山活動與火成岩。自然科學博物館，共300頁。 陳文山、王源，1996。臺灣東部海岸山脈地質。經濟部中央地質調查所，共101頁。 陳正宏、劉聰桂、楊燦堯、陳于高，1994。五萬分之一台灣地質圖說明書第65號-綠島。經濟部中央地質調查所，共57頁。 楊燦堯，1987。台灣東部海岸山脈奇美火成雜岩之岩石化學及核飛跡定年研究：國立台灣大學地質學研究所碩士論文，共123頁。 楊燦堯，1992。北呂宋島弧岩漿之演化及其地體構造模式：國立台灣大學地質學研究所博士論文，共458頁。 楊燦堯，2000。陽明山國家公園大屯火山群噴氣之氦同位素比值研究：國家公園學報，10(1)：73-94頁。 曹恕中，1992。新設立之鉀氬定年系統：經濟部中央地質調查所彙刊，第八號，63-97頁。 鍾孫霖，1990。台灣西部鹼性玄武岩中偉晶與包裹體之地球化學研究兼論晚新生代中國東南沿海板塊內部玄武岩的岩石成因：國立台灣大學地質學研究所博士論文，共183頁。 Ballentine, C. J. and Burnard, P. G., 2002. Production, release and transport of noble gases in the continental crust. Reviews in mineralogy & geochemistry, 47: 481-529. Chen, C. H., 1982. Petrological and geochemical study of the shoshonitic rocks of the Kuanyinshan area, northern Taiwan. Acta Geologica Taiwanica, 21: 33-62. Chen, C. H. and Tung, T. C., 1984. On-line data reduction for electron micro-probe analysis. Acta Geologica Taiwanica, 22: 196-200. Chen, C. H., Shieh, Y. N., Lee, T. Chen, C. H. and Mertzman, S. A., 1990. Nd-Sr-O isotopic evidence for source contamination and an unusual mantle component under Luzon Arc. Geochimica et Cosmochimica Acta, 54: 3476-2483. Chen, C. H., Lee, T. Shieh, Y. N. Chen, C. H. and Hsu, W. Y., 1995. Magmatism at the onset of back-arc basin spreading in the Okinawa Trough. Journal of Volcanoloyg and Geothermal Research, 69: 313-322. Chen, P. F., Huang, B. S. and Liang, W. T., 2004. Evidence of a slab of subducted lithosphere beneath central Taiwan from seismic waveforms and travel times. Earth and Planetary Science Letters, 229: 61-71. Chi, W. R., Namson, J. and Mei, W. W., 1980. Calcareous nannoplankton biostratigraphy of the Neogene sediment exposed along the Hsinkuluanchi in the Coastal Range, eastern Taiwan. Petroleum Geoogy of Taiwan, 17: 75-87. Graham, D. W., 2002. Nobles gas isotope geochemistry of mid-ocean ridge and ocean island basalt: characterization of mantle source reservoirs. Reviews in mineralogy & geochemistry, 47: 247-305. Hart, S. R., Blusztajn, J., Dick, H. J. B., Meyer, P. S. and Muehlenbachs, K., 1999. The fingerprint of seawater circulation in a 500-meter section of ocean crust gabbros. Geochimica et Cosmochimica Acta, 63: 4059-4080. Hilton, D. R., Hoogewerff, J. A., Bergen, M. J. A. and Hammerschmidt, K., 1992. Mapping magma source in the east Sunda-Banda arcs, Indonesia: Constrains from helium isotopes. Geochimica et Cosmochimica Acta, 56: 851-859. Hilton, D. R., Fischer, T. P. and Marty, B., 2002. Noble gases and volatile recycling at subduction zones. Reviews in mineralogy & geochemistry, 47: 319-362. Ho, K. S., Chen, J. C., Smith, A. D. and Juang, W. S., 2000. Petrogenesis of two group of pyroxenite from Tungchihsu, Penghu Island, Taiwan Strait: implications for mantle metasomatism beneath SE China. Chemical Geology, 167: 355-372. Honda, M., Phillips, D., Harris, J. W. and Yatsevich, I., 2004. Unusual noble gas compositions in polycrystalline diamonds: preliminary results from the Jwaneng kimberlite, Botswana. Chemical Geology, 203: 347-358. Hwang, W. T. and Lo, H. J., 1986. Volcanological aspects and the petrogenesis of the Kuanyinshan volcanic rocks, northern Taiwan. Acta Geologica Taiwanica, 24: 123-148. Kelley, S., 2002. K-Ar and Ar-Ar dating. Reviews in mineralogy & geochemistry, 47: 785-810. Kurz, M. D., 1986. Cosmogenic helium in a terrestrial rock. Nature, 320: 435-439. Lo, C. H. and Lee, C.Y., 1994. 40Ar/39Ar method of K-Ar age determination of geological samples using Tsing-Hua Open-Pool (THOR) reactor. Journal of the Geological Society of China, 37(2): 143-164. Lo, C. H., Wang, P. L., Yang, H. C., Liou, Y. S. and Tsou, T. Y., 2001. The laser 40Ar/39Ar dating microprobe of National Taiwan University. Western Pacific Earth Sciences, 1: 143-156. Lott, D.E., 2001. Improvements in noble gas separation methodology: A nude cryogenic trap. Geochemistry Geophysics Geosystems, 2: 2001GC00202. Matsuda, J., Matsumoto, T., Sumino, H., Nagao, K., Yammaoto, J., Miura, Y., Kaneoka, I., Takahata, N. and Sano, Y., 2001. The 3He/4He ratio of the new internal He Standard of Japan (HESJ). Geochemical Journal, 36: 191-195. Matsumoto, T., Honda, M., McDougall, I., O'Reilly, S. Y., Norman, M. and Yaxley, G., 2000. Noble gases in pyroxenites and metasomatised peridotites from the Newer Volcanics, southeastern Australia: implications for mantle metasomatism. Chemical Geology, 168: 49-73. Miura, Y.. and Nagao, K., 1991. Noble gases in six GSJ igneous rock samples. Geochemical Journal, 25: 163-171. Ozima, M. and Podosek, F. A., 2002. Noble gas geochemistry. Cambridge University Press, 281p. Poreda, R. and Craig, H., 1989. Helium isotope ratios in Circum-Pacific volcanic arcs. Nature, 338: 473-478. Salters, V. and Stracke, A. ,2004. Composition of the depleted mantle. Geochemistry, Geophysics, Geosystems, 5(5): doi: 10.1029/2003GC000597. Sarda, P., Staudacher, T., Allegre, C. J. and Lecomte, A., 1993. Cosmogenic neon and helium at Reunion: measurement of erosion rate. Earth and Planetry Science Letter, 119: 405-417. Scarsi, P., 2000. Fractional extraction of helium by crushing of olivine and clinopyroxene phenocrysts: Effects on the 3He/4He measured ratio. Geochimical Cosmochimica Acta, 64(21): 3751-3762. Soest, M. C. V., Hilton, D. R., Macpherson, G. G. and Mattey, D. P., 2002. Resolving sediment subduction and crustal contamination in the Lesser Antilles Island Arc: a combined He-O-Sr isotopes approach. Journal of Petrology, 43: 143-170. Song, S. R. and Lo, H. J., 2002. Lithofacies of volcanic rocks in the central Coastal Range, eastern Taiwan and their implications to the oceanic island arc evolution. Journal of Asia Earth Sciences, 21: 23-38. Teng, L. S., 1990. Geotectonic evolution of late Cenozoic arc-continent collision in Taiwan. Tectonophysics, 183: 57-76. Toyoda, S. and Ozima, M., 1988. Investigation of excess 4He and 40Ar in beryl by laser extraction technique. Earth and Planetry Science Letter, 90: 69-76. Wang, K. L., O'Reilly, S. Y., Griffin, W. L., Chung, S. L. and Pearson, N. J., 2003. Proterozoic mantle lithosphere beneath the extended margin of the south China block: In situ Re-Os evidence. Geology, 31(8): 709-712. Wang, K. L., Chung, S. L., O'Reilly, S. Y., Sun, S. S., Shinjo, R. and Chen, C. H., 2004. Geochemical constraints for the genesis of post-collisional magmatism and the geodynamic evolution of the northern Taiwan region. Journal of Petrology, 45(5): 975-1011. Wang, W. H. and Chen, C. H., 1990. The volcanology and fission track age dating of pyroclastic deposits in Tatun Volcano Group. Acta Geologica Taiwanica, 28:1-30. Xu, S., Nagao, K., Uto, K., Wakita, H. and Nakai, S., 1998. He, Sr and Nd isotopes of mantle-derived xenoliths in volcanic rocks of NE China. Journal of Asian Earth Sciences, 16(5-6): 547-556. Yamamoto, J., Kaneoka, I., Nakai, S., Kagi, H., Prikhod’ko, V. S. and Arai, S., 2004. Evidence for subduction-related components in the subcontinental mantle from low 3He/4He and 40Ar/36Ar ratio in mantle xenoliths from Far Eastern Russia. Chemical Geology, 207: 237-259. Yang, T. Y., Liu, T. K. and Chen, C. H., 1988. Thermal event records of the Chimei Igneous Complex: constraint on the ages of magma activities and the structural implication based on fission-track dating. Acta Geologica Taiwanica, 26: 237-246. Yang, T. F., Tien, J. L., Chen, C. H., Lee, T. and Punongbayan, R. S., 1995. Fission-track dating of volcanics in the northern part of the Taiwan-Luzon arc: eruption ages and evidence for crustal contamination. Journal of Southeast Asia Earth Sciences, 11(2): 81-93. Yang, T. F., Yang, C. C., Lee, C. Y., Chung, S. L. and Chen, C-H, 1996. NTUG rock standards for geochemical analysis. Journal of the Geological Society of China, 39: 307-323. Yang, T. F., Sano, Y. and Song, S. R., 1999. 3He/4He ratio of fumaroles and bubbling gases of hot springs in Tatun volcano Group, North Taiwan. Il Nuovo Cimento, 22(C): 281-286. Yang, T. F., Chen, C. H., Tien R. L., Song, S. R. and Liu, T. K., 2003. Remnant magmatic activity in the Coastal Range of East Taiwan after arc continent collision: Fission-track data and 3He/4He ratio evidence. Radiation Measurements, 36: 343 –349. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/36819 | - |
| dc.description.abstract | 稀有氣體同位素在地球科學及定年學皆有廣泛的應用，包含岩石成因、地體構造、礦物定年等。可應用的樣本分為氣體、液體、及固體三種，各有著不同的純化與分析步驟。目前台灣大學氣體地球化學實驗室已完成氣體及液體的稀有氣體分析純化系統，唯尚未設立固體樣本的分析系統，本研究目的為建立一套固體樣本的分析系統，以進一步討論其分析結果之意義。
為了使稀有氣體從固體樣本中釋出並進行分析，本研究使用電阻加熱式真空高溫爐，可應用的固體樣本有岩石樣本及礦物顆粒等，在高真空環境下階段式加熱樣本，使其逐段釋出稀有氣體，並經由純化線純化，及超低溫幫浦富集，再導入稀有氣體質譜儀分析其同位素比值。本研究針對稀有氣體中的氦(helium)、氬(argon)同位素進行分析，氦氣為分析3He及4He兩種同位素，而氬氣部分針對較常用的36Ar及40Ar進行實驗；分析得到之同位素比值則利用標準空氣與人工合成標準氣體，進行分析結果之校正。 本研究初步分析了台灣大學標準岩石樣本及6種礦物樣本。台灣大學標準岩石樣本的4He含量介於16.7~9087 nccSTP/g，3He/4He比值為0.00002~0.028Ra (Ra為大氣中的3He/4He比值，1.39×10-6)。六種礦物樣本分別是：中國漢諾壩橄欖石、澎湖橄欖石、觀音山斜輝石、嶺頂斜輝石，綠島斜輝石及綠島堇青石。礦物樣本的4He含量介於2.34∼10.64 nccSTP/g，3He/4He比值為1.12~7.04Ra。 氦氣含量及同位素分析結果顯示台灣大學標準岩石樣本樣本皆受到風化作用或是研磨過程影響，已經失去了90%左右的氦氣。嶺頂橄欖石為受到脫氣作用影響，而使4He含量及3He/4He比值皆降低；澎湖橄欖石之3He/4He比值與世界中洋脊玄武岩（MORB）之平均值相近；中國漢諾壩橄欖石之3He/4He比值和其他文獻比較，表現出相當大的異質性。觀音山斜輝石、綠島斜輝石及綠島堇青石等樣品之氦同位素比值分析結果均指出有地殼混染的訊號。 綠島岩漿成因長久以來存在有地殼混染或是源區混染的爭論，本研究利用綠島斜輝石及堇青石巨晶的3He/4He比值及其母岩漿的87Sr/86Sr比值，得到了綠島岩漿經歷過5%左右地殼混染的結果。配合上岩石學的觀察，本研究推論綠島火成岩曾受到地殼混染作用影響，而產生低3He/4He比值、高鍶同位素及低釹同位素比值的地化特性。 | zh_TW |
| dc.description.abstract | Noble gases isotopes are generally applied to chronology and geosciences, including petrology, tectonics, mineral dating and so on. Three types of samples can be analyzed, including gas, liquid and solid samples. There are different purification and analytic procedures for those samples. The procedures for gas and liquid samples are well established in NTU geochemistry laboratory. However, the procedures for solid samples are still not available. The aims of this research are to establish the analytic procedures for solid samples and to discuss the implications of those results.
To extract noble gases from solid samples, high-vacuum electric resistance heating furnace has been applied. Available samples of this study are rock powders and mineral crystals. Samples are transferred to the high-vacuum furnace, and heated with three steps of temperature. The extracted gas is purified and cryogenically concentrated. Helium concentration and isotopic composition are determined by mess spectrometer. 3He and 4He are analyzed for helium isotopes, while 36Ar and 40Ar are determined for argon isotopes. The isotopic results are calibrated by standard-air and artificial standard-gas. NTUG (National Taiwan University, Department of Geosciences) rock standards and six mineral samples are analyzed. Helium abundances of NTUG rock standards range from 16.7 to 9087 nccSTP/g, and helium ratios (3He/4He) range from 0.00002 to 0.028Ra (Ra is the helium ratio of air, 1.39×10-6). Six mineral samples are Hannuoba (漢諾壩) olivine of China, Penghu (澎湖) olivine, Kuanyinshan (觀音山) clino-pyroxene, Lingding (嶺頂) clino-pyroxene, Lutao (綠島) clino-pyroxene and cordierite. Helium abundances of mineral samples range from 2.34 to 10.64 nccSTP/g, and helium ratios (3He/4He) range from 1.12 to 7.04Ra. Helium abundances and ratios of NTUG rock standards show that those samples have lost approximately 90% of helium because of alteration or grinding. Helium ratio of Lingding olivine indicates helium degassing which decreases both helium ratio and concentration. Helium isotopic ratio of Penghu olivine shows MORB (Mid Ocean Ridge Basalt) value. Compared to previous study, Hannuoba samples show a wide range of 3He/4He ratios. Helium results of Kuanyinshan clino-pyroxene, Lutao clino-pyroxene and cordierite all indicate the signature of crust contamination. There is a long standing debate about the magma origin of Lutao. Two different models of crust contamination and source contamination are proposed. Combining helium results with strontium ratios of Lutao lavas, it shows that Lutao arc magma has experienced approximately 5% of crust contamination. In addition to available data, we can conclude that crust contamination of Lutao arc magma has resulted in low helium ratios, high strontium ratios and low neodymium ratios of Lutao lavas. | en |
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| dc.description.tableofcontents | 第一章 緒論................................................................................................................1
1-1 前言…………………………………………………………………………1 1-2 前人研究........................................................................................................2 第二章 採樣地點及樣本描述………………………………………………………3 2-1 岩石樣本……………………………………………………………………3 2-1-1 岩石粉末樣本分佈地點…………………………………………3 2-1-2 岩石粉末樣本成分及年代………………………………………4 2-2 礦物樣本……………………………………………………………………4 2-2-1 礦物樣本分佈地點………………………………………………4 2-2-2 礦物樣本描述……………………………………………………6 2-2-2-1 漢諾壩橄欖石(Hannuoba olivine)………………………….6 2-2-2-2 觀音山斜輝石(Kuanyinshan CPX) ………………..………7 2-2-2-3 嶺頂斜輝石(Lingding CPX)……..………...……………….7 2-2-2-4 綠島斜輝石及堇青石(Lutao CPX and cordierite)………....8 2-2-2-5 澎湖橄欖石(Penghu olivine)………………………….……9 2-2-3 礦物樣本成分……………………………………...…………….9 2-2-4 斜輝石礦物端成分圖………………………………………..…15 第三章 分析方法與研究原理………………………………………………………16 3-1 氦氣同位素………………………………………………………………..16 3-2 氦氣在礦物樣本中的保存位置…………………………………………..19 3-3 氬氣同位素………………………………………………………………..21 3-4 岩石及礦物樣本的分析流程……………………………………………..21 3-5 氣體萃取、純化及分析流程……………………………………………..23 第四章 分析結果……………………………………………………………………27 4-1 分析誤差…………………………………………………………………..27 4-2 分析極限…………………………………………………………………..28 4-3 分析結果…………………………………………………………………..30 4-3-1 NTUG標準岩石樣本分析結果………………………………..30 4-3-2 礦物標本分析結果……………………………………………..30 第五章 綜合討論……………………………………………………………………33 5-1 岩石粉末樣本分析結果之討論…………………………………………..33 5-1-1 岩石樣本4He含量之計算……………………………………...33 5-1-2 岩石樣本3He含量……………………………………………...35 5-1-3 岩石樣本之3He/4He比值………………………………………36 5-1-4 岩石樣本之岩石成因判別圖…………………………………..36 5-2 礦物樣本分析結果之討論………………………………………………..37 5-2-1 不同溫階下的氦氣行為………………………………………..37 5-2-2 礦物晶體與礦物粉末結果之比較……………………………..41 5-2-3 礦物樣本4He含量與3He/4He比值之關係……………………43 5-2-4 漢諾壩橄欖石分析結果之討論………………………………..44 5-2-5 嶺頂斜輝石分析結果之討論…………………………………..46 5-2-6 澎湖橄欖石分析結果之討論…………………………………..46 5-2-7 綠島堇青石分析結果之討論…………………………………..47 5-2-8 綠島斜輝石及觀音山斜輝石綠島堇青石分析結果之討論…..47 5-2-8-1 礦物樣本3He/4He比值降低之可能原因…………………48 5-2-8-2 世界上其他島弧岩漿具有地殼混染的例子……………..49 5-2-8-3 地殼及地函端源之氦氣比例……………………………..52 5-2-8-4 利用氦-鍶同位素判斷地殼混染或是源區混染………….52 5-3 綠島礦物樣本與噴氣樣本氦同位素比值之比較………………………..58 5-4 綠島岩漿生成模式示意圖………………………………………………..58 5-5 綠島岩漿氧同位素與氦同位素的不一致性……………………………..61 結論…………………………………………………………………………………..62 參考文獻……………………………………………………………………………..63 致謝…………………………………………………………………………………..67 | |
| dc.language.iso | zh-TW | |
| dc.subject | 固體樣本 | zh_TW |
| dc.subject | 氣體地球化學 | zh_TW |
| dc.subject | 稀有氣體 | zh_TW |
| dc.subject | 氦氣同位素 | zh_TW |
| dc.subject | noble gas | en |
| dc.subject | solid samples | en |
| dc.subject | helium isotope | en |
| dc.subject | gas geochemistry | en |
| dc.title | 固體樣本的稀有氣體同位素分析系統之建立與其應用 | zh_TW |
| dc.title | The Analyzing System for Noble Gas Isotopes on
Solid Samples and its Applications | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 93-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 陳中華,陳正宏,羅清華 | |
| dc.subject.keyword | 氣體地球化學,稀有氣體,氦氣同位素,固體樣本, | zh_TW |
| dc.subject.keyword | gas geochemistry,noble gas,helium isotope,solid samples, | en |
| dc.relation.page | 67 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2005-07-20 | |
| 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-94-1.pdf 未授權公開取用 | 4.03 MB | Adobe PDF |
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