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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 羅清華(Ching-Hwa Lo) | |
| dc.contributor.author | Jin-wei Hsu | en |
| dc.contributor.author | 許晉瑋 | zh_TW |
| dc.date.accessioned | 2021-06-15T05:57:50Z | - |
| dc.date.available | 2011-09-20 | |
| dc.date.copyright | 2010-08-20 | |
| dc.date.issued | 2010 | |
| dc.date.submitted | 2010-08-17 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/47393 | - |
| dc.description.abstract | 鮮水河斷層位於西藏高原東緣，截切了散佈著早中生代或新生代花岡岩體之古生代至早中生代沉積岩層。本研究沿鮮水河斷層採集花岡岩、偉晶岩與片麻岩岩石樣本，挑選鋯石、鉀長石與雲母類礦物進行鈾鉛定年與氬-氬定年研究，並結合熱年代學概念，以期了解鮮水河斷層帶活動歷史，並推論此區域大地構造演化意義。
各礦物樣本以人工挑選方式進行礦物分離，並以雷射階段加溫與雷射單礦物燒熔方式進行氬-氬定年分析。結果顯示雲母類礦物年代分布於兩群： 5.5-4.2 Ma與 153-141 Ma。採自貢嘎山地區之鉀長石年代約為4.4-4.2 Ma，而松潘甘孜地塊中的鉀長石則顯示了較老的年代 (142-44 Ma)。花岡岩中的鋯石鈾鉛定年結果則呈現了213+/-4 Ma，211+/-3 Ma與9.2+/-1.7 Ma之年代。 經計算各礦物之封存溫度，結合定年結果可推論出當地冷卻歷史與冷卻速率。並考慮前人所報導之鈾鉛、銣鍶與核飛跡年代後，研究結果顯示在貢嘎山地區自9 Ma起之冷卻速率高達100C/Myr，此外亦發現另一快速冷卻事件發生於14-9 Ma。其餘採自鮮水河斷層以北的花岡岩則呈現兩階段快速冷卻過程：第一階段為150-140 Ma前以約10C/Myr之速率冷卻，之後直至30-20 Ma後才以10C/Myr第二階段冷卻。然而，出露於鮮水河斷層以南的花岡岩僅於約140 Ma之前顯示一期快速冷卻事件。此結果表示在松潘甘孜地塊在侏儸紀期間曾發生侵蝕剝露事件 (至約150-140 Ma止)，印度歐亞間碰撞亦於松潘甘孜地塊東部導致再次抬升。 本研究成果顯示鮮水河斷層沿線之花岡岩體形成於早中生代，且曾經歷一段至早第三紀為止的長時間緩慢冷卻歷史。此外，來自貢嘎山之花岡岩、偉晶岩、片麻岩的年輕的氬-氬年代指出：鮮水河斷層之剪切運動確實發生於中新世與上新世，此運動反映了自從第三紀起始的印度-歐亞間碰撞。 | zh_TW |
| dc.description.abstract | In the eastern margin of the Tibet plateau, the Xianshuihe fault zone transacts Paleozoic-early Mesozoic sedimentary sequences which were intruded by a number of the Early Mesozoic or Cenozoic granites. Granite, pegmatite and gneiss samples were collected along the Xianshuihe fault zone for the present U-Pb and 40Ar/39Ar geochronological study, aiming to reveal the movement history for the fault zone and to explore its implications to regional tectonics.
The results show mica 40Ar/39Ar ages clustering in two groups: 5.5-4.2 Ma and 153-141 Ma. The younger ages appear in micas obtained from gneiss, granite and pegmatite in Kongashan, whereas the older ages were derived from granites in the Songpan-Garze fold belt. Two K-feldspars from granites in Kongashan display ages of 4.4+/-0.2 and 4.2+/-0.3 Ma, while other K-feldspars from the granites collected from outcrops in the Songpan-Garze fold belt show much older ages as 142+/-3 Ma, 70.6+/-1.8 Ma and 44.1+/-1.8 Ma. However, these 40Ar/39Ar ages are still much younger than their respective zircon U-Pb ages (213+/-4 Ma, 211+/-3 Ma) except one with 9.2+/-1.7 Ma. Considering their respective closure temperatures, these radiometric ages would indicate a cooling rate of 100C/Myr for the Kongashan area since ca. 9 Ma. The granites collected from the outcrops north of Xianshuihe fault zone in Songpan-Garze fold belt show two stages of rapid cooling, with a rate of 10C/Myr prior to ca. 150-140 Ma and 10C/Myr after 30-20 Ma, respectively. Other granite from the outcrop south of Xianshuihe fault only displays one rapid cooling stage prior ca. 140 Ma. This would suggest that an erosion and exhumation event in the Songpan-Garze fold belt may have occurred in Early Cretaceous (ca. 150-140 Ma). The collision between India and Eurasia caused further uplift in the eastern Songpan-Garze fold belt during Late Oligocene-Miocene. The present thermochronological study suggests that the granitic rocks cropping out along the Xianshuihe fault zone may have emplaced in the Early Mesozoic and experienced a prolonged cooling history until the Late Tertiary. While, the young radiometric ages from granite, gneiss and pegmatite samples indicate that the shearing activity of the Xianshuihe fault zone most likely occurred in the Miocene and Pliocene, in response to the active India-Eurasia collision starting since Tertiary. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-15T05:57:50Z (GMT). No. of bitstreams: 1 ntu-99-R96224101-1.pdf: 2785248 bytes, checksum: a3cad5ae0ccb2e417ad9de88c6a6b076 (MD5) Previous issue date: 2010 | en |
| dc.description.tableofcontents | Committee Censorship (口試委員會審定書) i
Acknowedgment (誌謝) ii Abstract in Chinese (摘要) iii Abstract v Content vii List of Figures ix List of Tables x Chapter 1 Introduction 1 1.1 Xianshuihe Fault Zone 4 1.2 Previous Studies 7 1.3 Geological Background 8 1.3.1 Songpan-Garze Fold Belt 8 1.3.2 Kongashan Granitic Massif 9 1.3.3 Longmenshan Thrust 10 1.4 Study Purposes 11 1.5 Samples 11 Chapter 2 Analytical Methods 15 2.1 Samples Preparation 15 2.2 Theory of 40Ar/39Ar Dating Method 16 2.3 40Ar/39Ar Dating 19 2.3.1 Laser Ablation Methods 19 2.3.2 Data Correction and Presentation 20 2.4 Theory of Closure Temperature 23 Chapter 3 Analytical Results 27 3.1 Results of Laser Step-heating 27 3.1.1 Kongashan Granitic Massif 27 3.1.1.1 06XS04a Granite 27 3.1.1.2 06XS21a Pegmatite 28 3.1.1.3 06XS21b Gneiss 29 3.1.2 Granite in Songpan-Garze Fold Belt 33 3.1.2.1 06XS09 Granite 33 3.1.2.2 06XS12 Granite 33 3.1.2.3 06XS23 Granite 34 3.2 Results of Laser Single-grain Fusion Experiments 40 3.2.1 Kongashan Granitic Massif 40 3.2.1.1 Biotite of 06XS04a Granite 40 3.2.1.2 Muscovite of 06XS21a Pegmatite 40 3.2.1.3 Biotite of 06XS21b Gneiss 40 3.2.2 Granite in Songpan-Garze Fold Belt 41 3.2.2.1 Biotite of 06XS09 Granite 41 3.2.2.2 Muscovite of 06XS12 Granite 41 3.2.2.3 Biotite of 06XS12 Granite 41 3.2.2.4 Biotite 06XS23 Granite 41 3.3 Estimation of Closure Temperature 47 3.4 Summary 49 Chapter 4 Discussion 53 4.1 Cooling History of Xianshuihe Area 55 4.1.1 Kongashan 55 4.1.2 Songpan-Garze Fold Belt 58 4.2 Tectonic Implication 62 4.2.1 Tectonic Evolution of the Songpan-Garze Fold Belt 62 4.2.2 Shearing Evolution of the Xianshuihe Fault Zone 65 4.2.3 Summary 68 Chapter 5 Conclusions 71 References 73 Appendix 87 I. Analytical Results for Laser Step-heating Experiments 87 II. Analytical Results for Laser Single-grain Fusion Experiments 100 | |
| dc.language.iso | en | |
| dc.subject | 西藏高原 | zh_TW |
| dc.subject | 氬氬定年 | zh_TW |
| dc.subject | 鮮水河斷層帶 | zh_TW |
| dc.subject | 40Ar/39Ar dating | en |
| dc.subject | Xianshuihe fault zone | en |
| dc.subject | Tibet | en |
| dc.title | 西藏高原東緣鮮水河斷層帶熱定年學研究 | zh_TW |
| dc.title | 40Ar/39Ar Thermochronological Study of Xianshuihe Fault Zone, Eastern Tibet | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 98-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 鍾孫霖(Sun-Lin Chung),李通藝(Tong-Yi Lee),葉孟宛(Meng-Wan Yeh),李元希(Yuan-Hsi Lee) | |
| dc.subject.keyword | 氬氬定年,鮮水河斷層帶,西藏高原, | zh_TW |
| dc.subject.keyword | 40Ar/39Ar dating,Xianshuihe fault zone,Tibet, | en |
| dc.relation.page | 111 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2010-08-18 | |
| 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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