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    請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/103797


    題名: Megathrust earthquake potential of the Manila subduction systems revealed by the radial component of seismic moment tensors Mrr
    作者: 林靜怡;Lin, Jing-Yi;Wu, Wen-Nan;Lo, Chung-Liang
    貢獻者: 地球科學學院地球科學學系
    關鍵詞: Accumulation;atmospheric science;Compressive properties;Coupling;Crustal deformation;Deformation;Deformation mechanisms;Earthquakes;geology;geophysics;hydrology;Mathematical analysis;oceanic science;Seismic activity;Seismic engineering;Seismic response;space science;Stresses;Subduction;Subduction (geology);Tensors
    日期: 2015-12-01
    上傳時間: 2026-04-23 11:37:46 (UTC+8)
    出版者: Chinese Geoscience Union;Taiwan: 中華民國地球科學學會
    摘要: 摘要: We undertook an investigation of the seismic behavior of large earthquake and estimated the crustal deformation state in the northern Philippine area in terms of the radial component of seismic moment tensors (Mrr) distribution. Based upon these two analyses, the seismic potential of the Manila Trench has been assessed. Regarding the seismic characteristics of large earthquakes, results show that both the overriding and the subducting plates are under compressive stress before the main large events but are characterized by an extensional regime after mainshocks. In the northern Manila Trench area, the broad zone of extensional seismic activity along the trench and its neighboring areas shows a stress environment distinct from that of the interseismic environment of large earthquakes, suggesting that the plates are in a relaxed state instead of accumulating tectonic stress. Thus, the coupling between the two plates could be weak. Along the central Manila Trench, even though only few extensional earthquakes occurred near the trench, numerous negative Mrr events in the overriding plate indicate that the crust is affected by a dilatational regime and also suggests a relatively low coupling environment. In the southern Manila Trench, with the exception of a few extensional events that occurred locally in the Central Valley Basin, most earthquakes show compressive mechanisms. We suggest that a relatively high plate coupling exists along this portion of the trench and results in stress accumulation not only along the plate interface but also in its vicinity, within the subducting and overriding plates.
    出版者: Taiwan: 中華民國地球科學學會
    出版日期: 2015-12-01
    出處: TAO : Terrestrial, atmospheric, and oceanic sciences, 2015-12, Vol.26 (6), p.619-630
    資源來源: 華藝CEPS中文電子期刊服務
    版權: 2015. This work is licensed under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
    識別號: ISSN: 1017-0839
    識別號: ISSN: 2223-8964
    識別號: ISSN: 2311-7680
    識別號: EISSN: 2311-7680
    識別號: DOI: 10.3319/TAO.2013.04.29.01(TC)
    顯示於類別:[地球科學學系] 期刊論文

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