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NTIS 바로가기韓國鑛物學會誌 = Journal of the Mineralogical Society of Korea, v.32 no.4, 2019년, pp.235 - 247
이홍금 (경상대학교 지질과학과 및 기초과학연구소) , 박원영 (경상대학교 지질과학과 및 기초과학연구소) , 구효진 (경상대학교 지질과학과 및 기초과학연구소) , 최재영 (경상대학교 지질과학과 및 기초과학연구소) , 장정규 (경상대학교 지질과학과 및 기초과학연구소) , 조현구 (경상대학교 지질과학과 및 기초과학연구소)
The Central South Sea Mud (CSSM), developed in the Seomjin River estuary, is known to be supplied with sediments from Heuksan Mud Belt (HMB) and Seomjin River. However, in order to form a mud belt, more sediments must be supplied than supplied in the above areas. Therefore, research on additional so...
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핵심어 | 질문 | 논문에서 추출한 답변 |
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남해에는 어떤 해류가 흐르는가? | , 1996). 또한, 주변 해류에는 한반도 연안을 따라 흐르는 한국연안류(KCC, Korea Coastal Current)와 외해로부터 유입되는 대마난류(TWC, Tsushima Warm Current)가 있다(Fig. 1). | |
남해는 어떤 해안으로 분류되는가? | 남해(South Sea)는 한반도 남서부의 흑산도, 동쪽의 대마도, 남쪽으로 제주도를 연결하는 한반도 남쪽 해역으로, 면적은 약 75,000 km2로 알려져 있다. 남해는 등수심선이 매우 복잡하게 발달되어 있는 리아스식 해안으로, 수심 70~80 m를 경계로 내대륙붕과 외대륙붕으로 구분된다(Park et al., 1990; Park et al. | |
남해란 무엇인가? | 남해(South Sea)는 한반도 남서부의 흑산도, 동쪽의 대마도, 남쪽으로 제주도를 연결하는 한반도 남쪽 해역으로, 면적은 약 75,000 km2로 알려져 있다. 남해는 등수심선이 매우 복잡하게 발달되어 있는 리아스식 해안으로, 수심 70~80 m를 경계로 내대륙붕과 외대륙붕으로 구분된다(Park et al. |
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