대만 중부지역의 3차원 속도구조

DC Field Value Language
dc.contributor.author 김광희 -
dc.contributor.author 유해수 -
dc.contributor.author 석봉출 -
dc.date.accessioned 2020-07-17T04:32:01Z -
dc.date.available 2020-07-17T04:32:01Z -
dc.date.created 2020-02-11 -
dc.date.issued 2007-04-26 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/30612 -
dc.description.abstract The destructive Mw 7.6 Chi-Chi earthquake shook the entire island of Taiwan on 21 September, 1999 (20 September 17:47 at UTC). The earthquake was followed by tremendous amount of aftershocks for the next a few months including ten strong aftershocks with magnitude greater than 6.0 (Figure 1). North-south trending about 85 km long surface rupture with vertical thrust and left lateral strike-slip offsets with the maximum 9.5 meters displacement was charted by field investigations. Here we show high resolution P- and S-wave velocity models in the devastating 1999 Chi-Chi, Taiwan, earthquake source area and its vicinity to understand the generating mechanism of the main shock and aftershock sequence. -
dc.description.uri 2 -
dc.language English -
dc.publisher 대한지질학회 -
dc.relation.isPartOf 2007년 춘계 지질과학기술 공동학술대회 -
dc.title 대만 중부지역의 3차원 속도구조 -
dc.title.alternative 3-D Velocity Models in the Central Taiwan Region -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 427 -
dc.citation.startPage 425 -
dc.citation.title 2007년 춘계 지질과학기술 공동학술대회 -
dc.identifier.bibliographicCitation 2007년 춘계 지질과학기술 공동학술대회, pp.425 - 427 -
dc.description.journalClass 2 -
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