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NTIS 바로가기바다 : 한국해양학회지 = The sea : the journal of the Korean society of oceanography, v.19 no.2, 2014년, pp.131 - 146
김소라 (부경대학교 에너지자원공학과) , 이광수 (한국지질자원연구원 석유해저연구본부) , 최동림 (한국해양과학기술원 남해특성연구부) , 김대철 (부경대학교 에너지자원공학과) , 이태희 (한국해양과학기술원 해양방위센터) , 서영교 (지마텍 주식회사)
High-resolution seismic profiles coupled with sediment sampling were analyzed to investigate the acoustic characters and distribution patterns of the late Holocene sediments in Gamak Bay of the South Sea, Korea. The mean grain size of surficial sediment lies around
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핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
가막만의 지리적 특징은? | 연구지역인 가막만은 한반도 남해안 중앙부에 위치하며, 주변 해역은 크고 작은 반도와 섬으로 형성된 내만이 잘 발달한 곳으로서 서측으로 여자만, 북측으로 광양만 그리고 동측으로 여수해만 등이 분포하고 있다(Fig. 1A). | |
가막만 형태는? | 1B). 만의 형태는 동서방향 9 km, 남북방향 15 km의 타원형 모양으로써, 만의 표면적이 112 km2, 해수용적 7.1×108m3으로 알려져있다(Kim et al., 2012). | |
음향기반암이란? | 음향기반암(Acoustic Basement): 가막만 지역에 나타나는 음향 기반암은 상부 퇴적층과 하부의 결정질 암석 사이를 구분하는 경계선이다. 탄성파 기록상에 나타나는 음향기반암의 양상은 매우 불규칙하며 기복이 심한 형태를 보이는데(Figs. |
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