博碩士論文 90222016 完整後設資料紀錄

DC 欄位 語言
DC.contributor物理學系zh_TW
DC.creator黃秉榮zh_TW
DC.creatorPing-Jung Huangen_US
dc.date.accessioned2003-7-15T07:39:07Z
dc.date.available2003-7-15T07:39:07Z
dc.date.issued2003
dc.identifier.urihttp://ir.lib.ncu.edu.tw:444/thesis/view_etd.asp?URN=90222016
dc.contributor.department物理學系zh_TW
DC.description國立中央大學zh_TW
DC.descriptionNational Central Universityen_US
dc.description.abstract地震發生時,所產生的能量與預期所要釋放出的能量低,因而,有自然學家推論地震發生時,滑動層中應存在單層的奈米級顆。而奈米級顆粒的存在,能使地震發生時所磨擦的能量減少。而本篇論文,發現到在921地震的滑動層中的確存在奈米級的顆粒,而奈米級的顆粒的最多的分佈範圍在10nm~40nm之間。另外,在X-光的繞射分析中,發現在滑動層中和滑動層的外圍的稜鐵礦(FeCO3)的強烈變化。在滑動層中,稜鐵礦在滑動層中,稜鐵礦幾乎消失不見,而碳酸鈣在地震的過程中,並沒太大變化,所以,推論在地震發生時滑動層當時的溫度介於兩者熔解溫度之間(580℃~894℃)。zh_TW
dc.description.abstractAtomic force microscopy (AFM) and General Structure Analysis System (GSAS) program have been used to investigate the nanometric characteristics of the fault gouge in the 223.45 m cores of Chi-Chi earthquake. Nano grains were revealed in the slip zone, with a mean diameter is ~20nm, while only μm grains were found outside the slip zone. X-ray diffraction patterns were refined following the Reiveld refinement method and reveal three main structural phases, namely quartz (hexagonal P6222 symmetry of SiO2), siderite (R-3CH symmetry of FeCO3), and calcite (R –3cRS symmetry of CaCO3), respectively. Among them, FeCO3 shows a rapidly percentage reduction from being at 35% to at 4 % as the specimen were taken from depths of 223.37 m (outside of the fault gouge) to 224.45 m (the fault gouge), while the composition of CaCO3 remains essentially unchanged. This founding can be used as an indicator for the temperature of the slip zone during the earthquake.en_US
DC.subject921zh_TW
DC.subject921en_US
DC.title921斷層泥中奈米礦物微粒的探尋 與滑動時地層溫度標定zh_TW
dc.language.isozh-TWzh-TW
DC.titleNanometric characteristics of fault gouge on the Chi-Chi earthquake, Taiwan en_US
DC.type博碩士論文zh_TW
DC.typethesisen_US
DC.publisherNational Central Universityen_US

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