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대한해협 해저사퇴 심부코어 SSDP-101의 퇴적상과 퇴적환경
Sedimentary Facies and Environments of the SSDP-101 Long-core in a Submarine Sand Ridge in the Korea Strait 원문보기

한국지구과학회지 = Journal of the Korean Earth Science Society, v.44 no.5, 2023년, pp.442 - 455  

김성필 (한국지질자원연구원 해저지질에너지연구본부) ,  양우헌 (전북대학교 과학교육학부)

초록
AI-Helper 아이콘AI-Helper

대한해협 대륙붕 해저사퇴의 형성과정을 이해하기 위해 77 m 심도 심부 SSDP-101 코어를 연구하였다. 이 심부코어는 WGS 측지계 기준으로 북위 128도 16.335분, 동경 34도 19.666분에 위치한 수심 60 m의 사퇴 정상부에서 시추하였다. SSDP-101 코어 시료의 해양지질학적 분석은 제4기 후기 상대 해수면 변화에 의해 야기된 대한해협 대륙붕 퇴적환경의 변화를 밝혔다. 하부 코어 퇴적층은 간헐적 하천 범람이 일어나는 염하구 환경에서 형성된 것으로 해석되었다. 연구 지역의 사퇴는 상대해수면이 현재보다 더 낮은 시기에 형성되었고, 사퇴 퇴적물은 상대해수면이 상승함에 따라 키질작용을 받았다. 현재 대륙붕의 해저사퇴는 해수면이 낮았던 시기의 해저사퇴가 현재 해수면 환경까지 잔존된 결과로 해석된다.

Abstract ▼ AI-Helper 아이콘AI-Helper

A long core SSDP-101 of 77 m in a submarine sand ridge on the Korea Strait shelf was studied to understand the formation process of the sand ridge. The long core was drilled at 128°16.335'N in latitude and 34°19.666'E in longitude (WGS-84) on the top of the sand ridge of 60-m water dep...

주제어

#대한해협   #SSDP-101 심부코어 시료   #해저사퇴   #퇴적환경  

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