博碩士論文 106322050 完整後設資料紀錄

DC 欄位 語言
DC.contributor土木工程學系zh_TW
DC.creator林佩蓉zh_TW
DC.creatorPei-Rong Linen_US
dc.date.accessioned2019-7-23T07:39:07Z
dc.date.available2019-7-23T07:39:07Z
dc.date.issued2019
dc.identifier.urihttp://ir.lib.ncu.edu.tw:444/thesis/view_etd.asp?URN=106322050
dc.contributor.department土木工程學系zh_TW
DC.description國立中央大學zh_TW
DC.descriptionNational Central Universityen_US
dc.description.abstract本研究資料來源為台灣中央氣象局地震資料庫,擷取西元1990年至2003年之地震目錄,首先利用 MATLAB 程式繪製四年內之地震分布圖,由較大規模之地震,例如芮氏規模6開始持續一點點的下降,從地震分布圖中找出距離近似均勻之5個地震事件,且誤差 ≦1.2% ,並記錄這些點組成的弧線以及其交叉,如無法找到,則將芮氏規模 M 慢慢下修直至找出地震圓弧線及其交叉,而此交叉我們稱之為「最強地震圓弧交叉」。 最強地震圓弧交叉形成後3年內,在交叉點向外延伸半徑90公里內及半徑70公里內,發生 M≧5.7 之強震機率:在半徑 90公里和300天內約有 75.0%,200天內約有 62.5%,100天內約有 62.5%;在半徑70公里和300天內約有 58.3%,200天內約有 50.0%,100天內約有 37.5%。發生規模 M≧6.0 之大地震機率:在半徑90公里和300天內約有 50.0%,200天內約有 33.3%,100天內約有 16.7%;半徑在70公里和300天內約有 33.3%,200天內約有 29.2%,100天內約有 12.5%。 最強地震圓弧雙交叉形成後3年內,在交叉點向外延伸半徑90公里內及半徑70公里內,發生M≧5.7 之強震機率:在半徑 90公里和300天內約有 76.9%,200天內約有 69.2%,100天內約有 46.2%;在70公里和300天內約有 69.2%,200天內約有 61.5%,100天內約有 38.5%;發生規模 M≧6.0 之大地震機率;在90公里和300天內約有 53.8%,200天內約有 53.8%,100天內約有 23.1%;在70公里和300天內約有 46.2%,200天內約有 46.2%,100天內約有 15.4%。 最強地震圓弧雙凸交叉形成後3年內,在交叉點向外延伸半徑90公里內及半徑70公里內,發生M≧5.7 之強震機率:在半徑 90公里和300天內約有 87.5%,200天內約有 87.5%,100天內約有 62.5%;在70公里和300天內約有 75.0%,200天內約有 75.0%,100天內約有 50.0%;發生規模 M≧6.0 之大地震機率:在90公里和300天內約有 62.5%,200天內約有 62.5%,100天內約有 25.0%;在70公里和300天內約有 50.0%,200天內約有 50.0%,100天內約有 12.5%。 zh_TW
dc.description.abstractThe data of this research’s is obtained from the seismic database of the Central Weather Bureau of Taiwan. The time range of analysis is from 1990 to 2003. We first use the MATLAB program to find the earthquakes with magnitudes of M≧6.0 in three years, and plot the seismic distribution .Next we try to find 5 earthquake events with uniform distances, and the error of the uniformity is required to be smaller than 1.2%. If no arc can be found, then we reduce the value of M to continue the search until an intersection of two circular arcs of earthquake can be found. This intersection is called " the strongest intersection of circular arcs of earthquakes ". In 3 years after “the strongest intersection of circular arcs of earthquakes” have occurred, we look for the strong earthquakes happened within the radius of 90 km and the radius of 70 km from the intersection. For the strong earthquakes of M≧5.7 , the occurrence probability in the circular regions with radii of 90 km is 75.0% in 300 days, 62.5% in 200 days, and 62.5% in 100 days. Inside the circular regions with radii of 70 kilometers, the occurrence probability is 58.3% in 300 days, 50.0% in 200 days, and 37.5% in 100 days. For the strong earthquakes of M≧6.0 , the occurrence probability in the circular regions with radii of 90 km is 50.0% in 300 days, 33.3% in 200 days, and 16.7% in 100 days. Inside the circular regions with radii of 70 kilometers, the occurrence probability is 33.3% in 300 days, 29.2% in 200 days, and 12.5% in 100 days. In 3 years after “the strongest double-convex intersection of circular arcs of earthquakes” have occurred, we look for the strong earthquakes happened within the radius of 90 km and the radius of 70 km from the intersection. For the strong earthquakes of M≧5.7 , the occurrence probability in the circular regions with radii of 90 km is 76.9% in 300 days, 69.2% in 200 days, and 46.2% in 100 days. Inside the circular regions with radii of 70 kilometers the occurrence probability is 69.2% in 300 days, 61.5% in 200 days, and 38.5% in 100 days. For the strong earthquake of M≧6.0 , the occurrence probability in the circular regions with radii of 90 km is 53.8% in 300 days, 53.8% in 200 days, and 23.1% in 100 days. Inside the circular regions with radii of 70 kilometers the occurrence probability is 46.2% in 300 days, 46.2% in 200 days, and 15.4% in 100 days. In 3 years after “the strongest double-convex intersection of circular arcs of earthquakes” have occurred, we look for the strong earthquakes happened within the radius of 90 km and the radius of 70 km from the intersection. For the strong earthquakes of M≧5.7 , the occurrence probability in the circular regions with radii of 90 km is 87.5% in 300 days, 87.5% in 200 days, and 62.5% in 100 days. Inside the circular regions with radii of 70 kilometers the occurrence probability is 75.0% in 300 days, 75.0% in 200 days, and 50.0% in 100 days. For the strong earthquakes of M≧6.0 , the occurrence probability in the circular regions with radii of 90 km is 62.5% un 300 days, 62.5% in 200 days, and 25.0% in 100 days. Inside the circular regions with radii of 70 kilometers the occurrence probability is 50.0% in 300 days, 50.0% in 200 days, and 12.5% in 100 days. en_US
DC.subject最強地震圓弧交叉zh_TW
DC.subject最強地震圓弧雙交叉zh_TW
DC.subject地震預測zh_TW
DC.subjectthe strongest intersection of circular arcs of earthquakesen_US
DC.subjectthe strongest double-convex intersection of circular arcs of earthquakesen_US
DC.subjectearthquake predictionen_US
DC.title台灣極淺層最強地震圓弧交叉與後續強震之關聯(1990年至2003年)zh_TW
dc.language.isozh-TWzh-TW
DC.type博碩士論文zh_TW
DC.typethesisen_US
DC.publisherNational Central Universityen_US

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