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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 陳勁吾 | |
| dc.contributor.author | Chih-Wei Cheng | en |
| dc.contributor.author | 鄭至為 | zh_TW |
| dc.date.accessioned | 2021-06-17T01:17:31Z | - |
| dc.date.available | 2019-08-25 | |
| dc.date.copyright | 2017-08-25 | |
| dc.date.issued | 2017 | |
| dc.date.submitted | 2017-08-14 | |
| dc.identifier.citation | Ammon, C. J. (1991), The isolation of receiver effects from teleseismic P waveforms, Bull. Seismol. Soc. Am., 81(6), 2504-2510.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/67022 | - |
| dc.description.abstract | 大屯火山群 (Tatun Volcano Group) 位於臺灣最北端區域，因沖繩海槽之前緣向西延伸擴張造成北台灣由過去擠壓應力環境轉變成拉張環境，形成造山崩解而噴發熔岩流之複式火山，其主要噴發年代為80至20萬年前，約至10萬年前噴發活動漸趨停止。根據鑽井資料分析，雖有多處火山噴發，但為同一岩漿來源。此區域之微震集中於深度小於5 公里的淺部，一般認為與熱水或氣體通過重力斷層、裂隙的造成壓力突變有關。近期研究發現大屯火山群東北方底下 ~20公里有岩漿庫。我們分析大屯火山觀測站 (Taiwan Volcano Observatory at Tatun) 寬頻地震站陣列的遠震波形資料，進一步探討大屯火山及鄰近區域底下之地殼構造。我們利用遠震P波接收函數法 (receiver functions) 約制地殼中的速度不連續面及莫荷面。我們分析2012至2013年間，震央距30至90度，規模大於6.0之遠震事件，由時間域迭代法 (iterative deconvolution) 計算接收函數。觀察Ps轉型波相及複反射訊號的到時與波形特徵。結果發現大屯火山區域莫荷面深度約為30公里，由西向東有漸深的趨勢，至東南方五分山測站一帶又變淺。Vp/Vs值於七星山及大屯火山群東北方約1.76至2，推測地殼溫度偏高，在大屯火山群東北方區域約20至25公里有一明顯低速層，推測是火成岩脈之部分熔融體。此外，大屯火山群東北方與東南方地殼可能存在非均向性，暗示地殼仍受到熱的作用，而在東南方地殼中有傾斜不連續面的訊號，應與火山活動有密切關聯。 | zh_TW |
| dc.description.abstract | The Tatun volcano group (TVG) in northern Taiwan was formed during the last 0.8 to 0.2 Ma thought to be associated with the turning of the regional stress from compression to tension between the arc-continent collision and subduction. The cause of eruption has been thought to mainly due to extensional collapse. The last is eruption estimated to occur ~6000 years ago. Post volcanic activities such as micro-earthquakes and gas emissions are still abundant and active in this region, especially near Tayoikeng areas. It has been long debated whether a magma chamber still exists beneath TVG. A recently study, proposed that a low-velocity zone, likely a magma reservoir, may reside in the lower crust beneath northern coast of Taiwan, to the northeast of TVG. To better image the crustal structure beneath TVG and its adjacent regions, we analyze waveform data recorded at 16 TVO (Taiwan Volcano Observatory at Tatun) dense broadband stations from 140 magnitude >6.0 teleseismic events during 2012-2013, generating receiver functions (RF) by time domain iterative deconvolution to detect seismic discontinuities. Our results show that the crustal structure in this region is heterogeneous and anisotropic likely due to the volcanic activities in the crust and cracks in the subsurface. The Ps converted phases are manifest at 3-4 s from most back-azimuth, indicating the presence of Moho discontinuity. The H-κ results confirm that the Moho is at 25-30 km across the region with increasing depth toward northeast, and the Vp/Vs ratio is 1.76-2 around ChiShin volcano. We further detect a low velocity zone layer to the northeast of TVG at ~22 km depth with thickness of 5 km, likely associated with volcanic activities. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-17T01:17:31Z (GMT). No. of bitstreams: 1 ntu-106-R04241313-1.pdf: 11406842 bytes, checksum: eec311ffd39c755e2ba8ca2e93517d19 (MD5) Previous issue date: 2017 | en |
| dc.description.tableofcontents | 口試委員會審定書...i
誌謝...ii 中文摘要...iii ABSTRACT...iv 目錄...v 圖目錄...viii 表目錄...xi 第一章 緒論...1 1.1 研究區域介紹...1 1.2 前人研究...5 1.2.1 大屯火山之形成...5 1.2.2 地球物理研究...6 1.3 研究動機與目的...18 1.4 本文論文內容...19 第二章 接收函數方法與原理...20 2.1 接收函數法原理...20 2.2 接收函數計算...23 2.3 時間域迭代之解迴旋法...25 2.4 H-κ疊加法...27 第三章 資料處理及分析...29 3.1 資料來源...29 3.2 接收函數之地震資料篩選與流程...33 3.3 疊加方法分析...41 3.3.1 自適應疊加法...41 3.3.2 隨後方位角變化疊加...44 3.3.3 隨震央距變化疊加...44 3.4 時間域解迴旋法之穩定度及參數設定...47 3.5 H-κ疊加法分析...50 第四章 研究結果與討論...54 4.1 東北方區域討論...59 4.1.1 莫荷面與速度構造...59 4.1.2 大屯火山群東北方之低速層...66 4.2 東南方區域莫荷面與速度構造討論...70 4.3 區域綜合討論...80 第五章 結論...88 參考文獻...89 附錄A 地震目錄...95 附錄B 各測站東南方區域H-κ結果...100 | |
| dc.language.iso | zh-TW | |
| dc.subject | 低速層 | zh_TW |
| dc.subject | 速度不連續面 | zh_TW |
| dc.subject | 接收函數 | zh_TW |
| dc.subject | 大屯火山群 | zh_TW |
| dc.subject | Tatun Volcano Group | en |
| dc.subject | receiver functions | en |
| dc.subject | crustal seismic discontinuities | en |
| dc.subject | low velocity zone | en |
| dc.title | 利用P波接收函數法探討台灣北部大屯火山群地殼速度不連續面 | zh_TW |
| dc.title | Crustal Seismic Discontinuities Beneath The Tatun Volcano Group in Northern Taiwan from P Receiver Functions | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 105-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 喬凌雲,曾泰琳,林正洪,梁文宗 | |
| dc.subject.keyword | 大屯火山群,接收函數,速度不連續面,低速層, | zh_TW |
| dc.subject.keyword | Tatun Volcano Group,receiver functions,crustal seismic discontinuities,low velocity zone, | en |
| dc.relation.page | 104 | |
| dc.identifier.doi | 10.6342/NTU201703185 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2017-08-14 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位： | 海洋研究所 | |
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