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NTIS 바로가기암석학회지 = The journal of the petrological society of korea, v.25 no.3, 2016년, pp.195 - 209
이진현 (부경대학교 지구환경과학과) , 권세현 (부경대학교 지구환경과학과) , 김영석 (부경대학교 지구환경과학과)
The understanding of geometric complexity of strike-slip Fault system can be an important factor to control fault reactivation and surface rupture propagation under the regional stress regime. The Kumamoto earthquake was caused by dextral reactivation of the Futagawa-Hinagu Fault system under the E-...
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핵심어 | 질문 | 논문에서 추출한 답변 |
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일본 열도와 한반도 사이의 지진발생 매커니즘을 규명하기 위해 필요한 것은? | 그러나 실질적으로 이러한 관계를 규명하는 것은 쉽지가 않다. 한반도는 지체구조적으로 태평양판뿐만 아니라 필리핀판과 인도판의 영향을 동시에 받는 것으로 해석 되고 있을 뿐만 아니라 이들 판경계와는 상당한 거리에 위치해 있기 때문에 이들 지진과 우리나라의 지진을 직접 연결하여 해석하기 위해서는 더 많은 추가적 인 자료가 필요하다. 그러나 만약 일본열도의 대지진과 한반도 내 지진활동에서 시공간적 관계가 존재한다면, 한반도에서 상대적으로 가까운 구마모토 지역에서 발생한 지진은 한반도 남동부 지역에서의 응력 변화 가능성과 활성단층의 재활 가능성 연구에 자극제가 될 수 있을 것이다. | |
2016년 4월 16일 발생한 지진은? | 2016년 4월 16일 일본 규슈 지역을 강타한 규모 7.1의 구마모토 지진 발생 이후, 2016년 7월 5일에는 울산 앞바다 52 km 해상에서 규모 5.0의 울산지진이 발생하였고, 9월 12일에는 규모 5. | |
구마모토 지진의 원인으로 추정되는 것은? | 특히, 구마모토 지진은 후타가와(Futagawa)-히나구 (Hinagu) 단층대의 우수향 재활에 의한 것으로 해석 되고 있으며, 이들 단층들은 동북동 방향의 후타가와 단층이 북북동 방향의 히나구단층에 서로 사교하며 접하는 λ-단층과 유사한 기하적인 형태를 가진다(Fig. 2). |
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