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Analysis of Paleo Sedimentary Environment of Gochang Coast Using Grain Size Distribution Characteristics

입도분포 특성을 기반으로 한 고창 연안의 과거 퇴적환경 분석

  • Han, Min (Geo-Environmental Hazards & Quaternary Geology Research Center, Korea Institute of Geoscience and Mineral Resources) ;
  • Yang, Dong-Yoon (Geo-Environmental Hazards & Quaternary Geology Research Center, Korea Institute of Geoscience and Mineral Resources) ;
  • Park, Chanhyeok (Department of Astronomy, Space Science and Geology, Chungnam National University)
  • 한민 (한국지질자원연구원 지질환경재해연구센터) ;
  • 양동윤 (한국지질자원연구원 지질환경재해연구센터) ;
  • 박찬혁 (충남대학교 우주.지질학과)
  • Received : 2018.08.06
  • Accepted : 2018.09.17
  • Published : 2018.09.30

Abstract

This study aimed to identify different sedimentary environments of Gochang coast according to geomorphic conditions of each bore hole. To achieve the aim, this study utilized the classification of sedimentary environmental conditions of surface sediment, which was based on grain size distribution characteristics.In other words, three sedimentary environmental conditions ofsandy flat + sand beach, coastal sand dune and weathered bedrock soil, which were distinguished based on grain size distribution characteristics of mean-sorting for surface sediments, were applied to the sediments of bore holes. Four sedimentary environments could be identified in Gochang coast. First, the lake sedimentary environment originated from terrestrial sediments seems to have been dominated by weathered bedrock soil that the surface flow has deposited in a coastal wetland or a boundary, which is affected by the sea. Second, the lake sedimentary environment that is little affected by coastal sand dunes is located at the center of a valley, which is connected to the land, and the dune slack of Saban-ri. The surface flow of weather bedrock soil is the main source of deposits. However, there seems to have been a temporary influence of the sea. Third, the lake sedimentary environment that is strongly affected by coastal sand dunes is located at the dune slack of Yeongjeong-ri. This environment shows traces of a change from a coastal sand dune into the dune slack. Finally, the coastalsand dune sedimentary environment, which wasinvestigated by boring the current coastal sand dune, shows a temporary influence of the land but seems to have maintained the overall stability. Consequently, this study demonstrated that the grain size distribution characteristics of the present surface sediments could be effectively applied to identify the sedimentary environments of the paleo bore hole sediments. In addition, the paleo change of sedimentary environment could also be identified in many places of Gochang coast. If the results of this study are combined with the age dating and geochemical analysis in future works, the paleo environmental change in Gochang coast will be restored more precisely.

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Acknowledgement

Grant : 기후변화 적응 산사태 조기경보기술 및 지질환경재해 리스크 제어기술 개발

Supported by : 한국해양과학기술진흥원