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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/987654321/103827


    題名: Multi-parametric investigation of the volcano-hydrothermal system at Tatun Volcano Group, Northern Taiwan
    作者: 柯士達;Rontogianni, S.;Konstantinou, K. I.;Lin, C.-H.
    貢獻者: 地球科學學院地球科學學系
    關鍵詞: Analysis;Earthquakes;General Earth and Planetary Sciences;Investigations;Magma;Seismic activity;Seismology;Volcanoes;Volcanology
    日期: 2012-08-10
    上傳時間: 2026-04-23 11:38:14 (UTC+8)
    出版者: European Geosciences Union;Katlenburg-Lindau: Copernicus Publications
    摘要: 摘要: The Tatun Volcano Group (TVG) is located in northern Taiwan near the capital Taipei. In this study we selected and analyzed almost four years (2004–2007) of its seismic activity. The seismic network established around TVG initially consisted of eight three-component seismic stations with this number increasing to twelve by 2007. Local seismicity mainly involved high frequency (HF) earthquakes occurring as isolated events or as part of spasmodic bursts. Mixed and low frequency (LF) events were observed during the same period but more rarely. During the analysis we estimated duration magnitudes for the HF earthquakes and used a probabilistic non-linear method to accurately locate all these events. The complex frequencies of LF events were also analyzed with the Sompi method indicating fluid compositions consistent with a misty or dusty gas. We juxtaposed these results with geochemical/temperature anomalies extracted from fumarole gas and rainfall levels covering a similar period. This comparison is interpreted in the context of a model proposed earlier for the volcano-hydrothermal system of TVG where fluids and magmatic gases ascend from a magma body that lies at around 7–8 km depth. Most HF earthquakes occur as a response to stresses induced by fluid circulation within a dense network of cracks pervading the upper crust at TVG. The largest ( M L ~ 3.1) HF event that occurred on 24 April 2006 at a depth of 5–6 km had source characteristics compatible with that of a tensile crack. It was followed by an enrichment in magmatic components of the fumarole gases as well as a fumarole temperature increase, and provides evidence for ascending fluids from a magma body into the shallow hydrothermal system. This detailed analysis and previous physical volcanology observations at TVG suggest that the region is volcanically active and that measures to mitigate potential hazards have to be considered by the local authorities.
    出版者: Katlenburg-Lindau: Copernicus Publications
    出版日期: 2012-07-19
    出處: Natural Hazards and Earth System Sciences, 2012-07, Vol.12 (7), p.2259-2270
    資源來源: Agricultural & Environmental Science Collection
    版權: COPYRIGHT 2012 Copernicus GmbH
    版權: Copyright Copernicus GmbH 2012
    識別號: ISSN: 1684-9981
    識別號: ISSN: 1561-8633
    識別號: EISSN: 1684-9981
    識別號: DOI: 10.5194/nhess-12-2259-2012
    顯示於類別:[地球科學學系] 期刊論文

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