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請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79256
完整後設資料紀錄
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dc.contributor.advisor胡植慶(Jyr-Ching Hu)
dc.contributor.authorYu-TIng Taien
dc.contributor.author戴郁庭zh_TW
dc.date.accessioned2022-11-23T08:56:47Z-
dc.date.available2022-02-21
dc.date.available2022-11-23T08:56:47Z-
dc.date.copyright2022-02-21
dc.date.issued2021
dc.date.submitted2022-01-17
dc.identifier.citation朱偉林、白國平、李勁松,2014,札格羅斯盆地。中東含油氣盆地,朱偉林主編,244-296,北京:科學出版社。 吳榮章、楊耿明、丁信修、蔡錦椿、王佳彬、梅文威,1995,地質剖面平衡電腦分析及其應用。鑛冶:中國鑛冶工程學會會刊,39(2),148-163。 吳笙緯,2019,應用小基線子集干涉技術探討六龜地區地表形變。交通大學土木工程系所學位論文,1-77。 陳采蔚,2016,苗栗地區錦水背斜地下構造演育與裂縫發育。台灣大學地質科學研究所學位論文,1-90。 賈小樂、何登發、童曉光,2013,札格羅斯前陸盆地大油氣田的形成條件與分布規律。中國石油勘探,18(5),54-67。 謝嘉聲,2006,以雷達干涉技術偵測地表變形之研究。國立交通大學土木工程學系博士論文,共159頁。 Alavi, M., Vaziri, H., Seyed-Emami, K., Lasemi, Y., 1997. The Triassic and associated rocks of the Nakhlak and Aghdarband areas in central and northeastern Iran as remnants of the southern Turanian active continental margin. Geol. Soc. Am. Bull., 109(12), 1563-1575, doi: 10.1130/0016-7606(1997)109<1563:TTAARO>2.3.CO;2. Alavi, M., 2004. Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution. Am. J. Sci., 304(1), 1-20, doi: 10.2475/ajs.304.1.1. Alavi, M., 2007. Structures of the Zagros fold-thrust belt in Iran. Am. J. Sci., 307(9), 1064-1095, doi: 10.2475/09.2007.02. Berardino, P., Fornaro, G., Lanari, R., Sansosti, E., 2002. A new algorithm for surface deformation monitoring based on small baseline differential SAR interferograms. IEEE Trans. Geosci. Remote Sens., 40(11), 2375-2383, doi: 10.1109/TGRS.2002.803792. Berberian, M., 1981. Active faulting and tectonics of Iran. In Zagros Hindu Kush Himalaya Geodynamic Evolution, Geodynamics Series, 33–69, edited by Gupta H. K., Delany F. M., doi:10.1029/gd003p0033. Burberry, C. M., Cosgrove, J. W., Liu, J. G., 2010. A study of fold characteristics and deformation style using the evolution of the land surface: Zagros Simply Folded Belt, Iran. Geol. Soc. Spec. Publ., 330(1), 139-154, doi: 10.1144/SP330.8. Carruba, S., Perotti, C. R., Buonaguro, R., Calabrò, R., Carpi, R., Naini, M., 2006. Structural pattern of the Zagros fold-and-thrust belt in the Dezful Embayment (SW Iran). Geol. Soc. Am. Spec. Pap., 414, 11, doi:10.1130/2006.2414(02). Costa, E., Vendeville, B., 2002. Experimental insights on the geometry and kinematics of fold-and-thrust belts above weak, viscous evaporitic décollement. J. Struct. Geol., 24(11), 1729-1739, doi: 10.1016/S0191-8141(01)00169-9. Derikvand, B., Alavi, S. A., Fard, I. A., Hajialibeigi, H., 2018. Folding style of the Dezful Embayment of Zagros Belt: Signatures of detachment horizons, deep-rooted faulting and syn-deformation deposition. Mar. Pet. Geol., 91, 501-518, doi: 10.1016/j.marpetgeo.2018.01.030. Esmaeili, B., Safikhani, A. A., Samani, A. A., 2012. Geotechnical consideration regarding the routing of twin railway tunnels across the Karoun River. WIT Transactions on The Built Environment, 128, 641-648. Falcon, N. L., 1969. Problems of the relationship between surface structure and deep displacements illustrated by the Zagros Range. Geol. Soc. Spec. Publ., 3(1), 9–21. doi:10.1144/gsl.sp.1969.003.01.02. Farahzadi, E., Alavi, S. A., Sherkati, S., Ghassemi, M. R., 2019. Variation of subsidence in the Dezful Embayment, SW Iran: influence of reactivated basement structures. Arab. J. Geosci., 12(19), 1-22, doi: 10.1007/s12517-019-4758-5. Hatzfeld, D., Authemayou, C., Van Der Beek, P., Bellier, O., Lavé, J., Oveisi, B., ... Yamini-Fard, F., 2010. The kinematics of the Zagros mountains (Iran). Geol. Soc. Spec. Publ., 330(1), 19-42, doi: 10.1144/SP330.3. Hessami, K., Nilforoushan, F., Talbot, C. J., 2006. Active deformation within the Zagros Mountains deduced from GPS measurements. J. Geol. Soc. London., 163(1), 143-148, doi: 10.1144/0016-764905-031. Karasözen, E., Nissen, E., Bergman, E. A., Ghods, A., 2019. Seismotectonics of the Zagros (Iran) from orogen‐wide, calibrated earthquake relocations. J. Geophys. Res. Solid Earth, 124(8), 9109-9129, doi: 10.1029/2019JB017336. Kavoosi, M. A., Sherkati, S., 2012. Depositional environments of the Kalhur Member evaporites and tectonosedimentary evolution of the Zagros fold–thrust belt during Early Miocene in south westernmost of Iran. Carbonates Evaporites, 27(1), 55-69, doi:10.1007/s13146-012-0084-7. Karimzadeh, S., Cakir, Z., Osmanoğlu, B., Schmalzle, G., Miyajima, M., Amiraslanzadeh, R., Djamour, Y., 2013. Interseismic strain accumulation across the North Tabriz Fault (NW Iran) deduced from InSAR time series. J. Geodyn., 66, 53-58, doi: 10.1016/j.jog.2013.02.003. Lillesand, T., R.W. Kiefer, J. Chipman, 2015. Remote sensing and image interpretation, 6th edition, Wiley, USA, 736p. Liu, X., Wen, Z., Wang, Z., Song, C., He, Z., 2018. Structural characteristics and main controlling factors on petroleum accumulation in Zagros Basin, Middle East. Nat. Gas Geosci., 3(5), 273-281, doi: 10.1016/j.jnggs.2018.11.004. Motagh, M., Bahroudi, A., Haghighi, M. H., Samsonov, S., Fielding, E., Wetzel, H. U., 2015. The 18 August 2014 M w 6.2 Mormori, Iran, earthquake: A thin‐skinned faulting in the Zagros Mountain inferred from InSAR measurements. Seismol. Res. Lett., 86(3), 775-782, doi: 10.1785/0220140222. McQuarrie, N., 2004. Crustal scale geometry of the Zagros fold–thrust belt, Iran. J. Struct. Geol., 26(3), 519-535, doi: 10.1016/j.jsg.2003.08.009. Najafi, M., Yassaghi, A., Bahroudi, A., Vergés, J., Sherkati, S., 2014. Impact of the Late Triassic Dashtak intermediate detachment horizon on anticline geometry in the Central Frontal Fars, SE Zagros fold belt, Iran. Mar. Pet. Geol., 54, 23-36, doi: 10.1016/j.marpetgeo.2014.02.010. Najafi, M., Vergés, J., Etemad‐Saeed, N., Karimnejad, H. R., 2018. Folding, thrusting and diapirism: Competing mechanisms for shaping the structure of the north Dezful Embayment, Zagros, Iran. Basin Res., 30(6), 1200-1229, doi: 10.1111/bre.12300. Najafi, M., Lajmorak, S., 2020. Contractional salt-tectonic system in the south Dezful embayment, Zagros. J. Struct. Geol., 141, 104204, doi: 10.1016/j.jsg.2020.104204. Pirouz, M., Avouac, J. P., Gualandi, A., Hassanzadeh, J., Sternai, P., 2017. Flexural bending of the Zagros foreland basin. Geophys. J. Int., 210(3), 1659-1680, doi: 10.1093/gji/ggx252. Roosta, H., Jalalifar, H., Nasab, S. K., Ranjbar, M., 2019. Seven years of surface deformation above the buried Nasr-Abad salt diapir using InSAR time-series analysis, Central Iran. J. Geodyn., 130, 1-11, doi: 10.1016/j.jog.2019.05.006. Safari, H. O., Pirasteh, S., Pradhan, B., Gharibvand, L. K., 2010. Use of remote sensing data and GIS tools for seismic hazard assessment for shallow oilfields and its impact on the settlements at Masjed-i-Soleiman Area, Zagros Mountains, Iran. Remote Sens., 2(5), 1364-1377, doi: 10.3390/rs2051364. Sepehr, M., Cosgrove, J. W., 2004. Structural framework of the Zagros fold–thrust belt, Iran. Mar. Pet. Geol., 21(7),829-843, doi: 10.1016/j.marpetgeo.2003.07.006. Sherkati, S., Letouzey, J., 2004. Variation of structural style and basin evolution in the central Zagros (Izeh zone and Dezful Embayment), Iran. Mar. Pet. Geol., 21(5), 535-554, doi: 10.1016/j.marpetgeo.2004.01.007. Sherkati, S., Molinaro, M., de Lamotte, D. F., Letouzey, J., 2005. Detachment folding in the Central and Eastern Zagros fold-belt (Iran): salt mobility, multiple detachments and late basement control. J. Struct. Geol., 27(9), 1680-1696, doi: 10.1016/j.jsg.2005.05.010. Sherkati, S., Letouzey, J., Frizon de Lamotte, D., 2006. Central Zagros fold‐thrust belt (Iran): New insights from seismic data, field observation, and sandbox modeling. Tectonics, 25(4), TC4007, doi: 10.1029/2004TC001766. Vergés, J., Saura, E., Casciello, E., Fernandez, M., Villaseñor, A., Jimenez-Munt, I., García-Castellanos, D., 2011. Crustal-scale cross-sections across the NW Zagros belt: Implications for the Arabian margin reconstruction. Geol. Mag., 148(5-6), 739-761, doi: 10.1017/S0016756811000331. Walpersdorf, A., Hatzfeld, D., Nankali, H., Tavakoli, F., Nilforoushan, F., Tatar, M., Vernant, P., Chéry, J., Masson, F., 2006. Difference in the GPS deformation pattern of North and Central Zagros (Iran). Geophys. J. Int., 167(3), 1077-1088, doi: 10.1111/j.1365-246X.2006.03147.x. Woodbridge, K. P., Parsons, D. R., Heyvaert, V. M., Walstra, J., Frostick, L. E., 2016. Characteristics of direct human impacts on the rivers Karun and Dez in lowland south-west Iran and their interactions with earth surface movements. Quat. Int., 392, 315-334, doi: 10.1016/j.quaint.2015.10.088. Zarifi, Z., Nilfouroushan, F., Raeesi, M., 2014. Crustal stress map of Iran: Insight from seismic and geodetic computations. Pure Appl. Geophys., 171(7), 1219-1236. Zhang, Y., Fattahi, H., Amelung, F., 2019. Small baseline InSAR time series analysis: Unwrapping error correction and noise reduction. Compu. Geosci., 133, 104331, doi: 10.1016/j.cageo.2019.104331.
dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79256-
dc.description.abstract札格羅斯盆地長約1400公里,100-300公里寬,從伊朗的東南方一路延伸至土耳其的東邊。阿拉伯板塊與歐亞板塊在始新世發生斜向聚合的陸-陸碰撞,形成高札格羅斯帶。札格羅斯盆地則在中新世時開始形成,現今兩個板塊的斜向碰撞速率大約是20-30 mm/yr。沉積環境以及構造的演化過程使這個盆地蘊含了豐富的油氣系統,在2009年時,已有至少60個油田與氣田被發現並開始探採油氣資源。了解札格羅斯盆地構造的演化為石油探勘的基礎,可幫助石油探採專業人員發掘可能油氣的生成時機與移棲的地點。由於札格羅斯盆地位於兩個板塊的交界帶上,地震活動頻繁,構造運動活躍,研究新構造的活動性,亦有助於了解札格羅斯盆地構造的演育。本研究數化前人所建立之地質剖面,並使用Move 2018進行地質剖面回復,探討前人建立之剖面合理性,並藉此了解構造的演化過程。此外,利用伊朗國家地震中心的地震資料去分析在剖面沿線上各構造的地震活動與構造之關聯,並利用合成孔徑雷達干涉時間序列分析對不同構造的地表變形進行觀測。根據剖面回復結果,斷層的主要演化包含了順序發育以及脫序發育,剖面的總縮短量大約為34公里。從地震資料分析,山前斷層(Mountain Front Fault,MFF)、納夫賽菲德背斜(Naft Safid Anticline)、馬斯吉德蘇萊曼背斜(Masjid-i-Soleyman Anticline,MIS Anticline)具有較顯著的活動性,其中山前斷層容納了9.6公里的縮短量,並導致卡馬倫背斜逐漸成為一斷層擴展褶皺。從地震資料分析與InSAR觀測,可觀察到變形從東北方傳向西南方的前陸盆地的現象,在西南方的前陸盆地地震相當活躍。利用InSAR的時間序列分解成垂直向與東西向的結果,可分析前陸盆地的主要構造活動。在近三年內,地表有較明顯變形行為的構造分別是阿瓦茲背斜(Ahwaz Anticline)、庫帕爾背斜(Kupal Anticline)、拉赫巴里斷層(Lahbari Fault),其中阿瓦茲背斜的變形行為與阿瓦茲斷層有極大的關聯。阿瓦茲背斜西南翼的水平向速度無太大變化,東北翼的速度變化為1 cm/yr;西南翼的垂直向速度變化小於0.5 cm/yr,東北翼為1 cm/yr。庫帕爾背斜水平向速度西南翼為0.3 cm/yr、東北翼小於0.3 cm/yr;西南翼的垂直向運動為0.7 cm/yr,東北翼為0.75 cm/yr。拉赫巴里斷層上、下盤的水平速度運動不明顯;在垂直向速度的部分上盤則相對於下盤抬升0.5 cm/yr。除此之外,亦可在合成孔徑雷達干涉的結果中,發現與河流有關的側向侵蝕與側向堆積現象所造成之地表地形的變形。zh_TW
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dc.description.tableofcontents國立臺灣大學碩士學位論文口試委員審定書 I 致謝 II 摘要 III Abstract V 目錄 VII 圖目錄 X 表目錄 XV 第一章 緒論 1 1.1 前言 1 1.2 前人研究 4 1.2.1 蒸發岩與其變形機制 4 1.2.2 地質構造剖面 11 1.2.3 板塊幾何模型的計算 18 1.2.4 小基線子集方法(Small BAseline Subset method,SBAS method) 20 第二章 地體構造與地質背景 26 2.1 盆地演化歷史 26 2.2 構造概況 29 2.3 研究區域 34 2.3.1地層概況 34 2.3.2地質構造 43 2.3.3活動構造 46 第三章 研究方法與資料 56 3.1 平衡剖面基本建立理論 56 3.1.1 地質剖面建立方法 56 3.1.2 斷層相關褶皺 58 3.1.3 地質剖面資料 61 3.2 平衡剖面之回復 65 3.2.1平衡原則 65 3.2.3回復方法 65 3.3 合成孔徑雷達干涉技術 67 3.3.1合成孔徑雷達 68 3.3.2合成孔徑雷達干涉 70 3.3.3小基線子集法時間序列 73 3.3.4小基線子集法研究流程 75 3.3.5 InSAR資料 77 第四章 研究成果 80 4.1 地質剖面構造解釋 80 4.2 剖面回復成果 84 4.2.1小型正斷層及庫帕爾背斜(Kupal Anticline)之回復(Step 1) 84 4.2.2泰木爾背斜(Ab-e-Teimur Anticline)之回復(Step 2) 85 4.2.3納夫塞菲德背斜(Naft Safid Anticline)之斷層回復(Step 3) 88 4.2.4拉敏背斜(Ramin Anticline)與斷層之回復(Step 4) 88 4.2.5阿瓦茲背斜(Ahwaz Anticline)與斷層之回復(Step 5) 88 4.2.6山前斷層(Mountain Frontal Fault)與加奇薩蘭層之回復(Step 6) 92 4.2.7馬斯吉德蘇萊曼背斜(Masjid-i-Soleyman Anticline)下方斷層回復(Step 7) 92 4.2.8納夫塞菲德背斜(Naft Safid Anticline)、馬斯吉德蘇萊曼背斜(Masjid-i-Soleyman Anticline)回復(Step 8) 95 4.2.9卡馬倫背斜(Kamarun Anticline)、卡馬斯坦背斜(Kamestan Anticline)回復(Step 9) 95 4.2.10庫馬列克斷層(Kuh-e-Malek Thrust)及庫馬列克背斜(Kuh-e-Malek Anticline)回復(Step 10) 95 4.3 小基線子集法之時間序列結果 100 第五章 討論 107 5.1 地層厚度側向變化 107 5.2 迪茲富勒的活動構造 111 5.2.1 地質剖面與活動構造 111 5.2.2 地震與活動構造 112 5.2.3 InSAR與活動構造 117 5.3 InSAR時間序列分析與地表地形關係 124 第六章 結論 127 參考文獻 129 附錄 133
dc.language.isozh-TW
dc.title應用平衡剖面及InSAR探討伊朗迪茲富勒構造演化及構造活動zh_TW
dc.titleStructural Evolution and Active Structures of Dezful Embayment in Zagros Foreland Basin Deduced from Balanced Cross Section and SAR Interferometryen
dc.date.schoolyear110-1
dc.description.degree碩士
dc.contributor.oralexamcommittee黃鐘(Yen-Chou Lin),賴光胤(Sheng-Jung Ou),蔡旻倩(Wan-Yu Chou),謝嘉聲(Po-Ju Chang)
dc.subject.keyword迪茲富勒弧凹,回復平衡剖面,滑脫面,合成孔徑雷達干涉技術,小基線子集法,zh_TW
dc.subject.keywordDezful embayment,Restore Cross Section,Detachment,InSAR,SBAS,en
dc.relation.page135
dc.identifier.doi10.6342/NTU202200045
dc.rights.note同意授權(全球公開)
dc.date.accepted2022-01-18
dc.contributor.author-college理學院zh_TW
dc.contributor.author-dept地質科學研究所zh_TW
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