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Fault-related Landforms and Geomorphological Processes Around Ungchon-Ungsang Areas in the Middle Part of the Dongrae Fault

동래 단층 중부 지역 웅촌-웅상 일대의 단층 지형과 지형 발달

  • Lee, Gwang-Ryul (Department of Geography Education, Kyungpook National University) ;
  • Park, Chung-Sun (Department of Geography, Kyungpook National University) ;
  • Shin, Jae Ryul (Department of Geography Education and Engineering Research Institute, Gyeongsang National University)
  • 이광률 (경북대학교 지리교육과) ;
  • 박충선 (경북대학교 지리학과) ;
  • 신재열 (경상대학교 지리교육과 및 공학연구원)
  • Received : 2019.02.28
  • Accepted : 2019.03.13
  • Published : 2019.03.30

Abstract

This study analyzed the distribution of fluvial landforms, fault-related geomorphic features and lineaments around the area of Ungchon-Ungsang in the Dongrae Fault, and discusses the charateristics of geomorphic development based on those. As a result, the NE-SW lineaments are predominantly developed in many numbers within the study area, and the NW-SE or N-S secondary lineaments are developed induced by multiple deformation with the Yangsan Fault. Geomorphologically, the early tectonic history of the Ungchon-Ungsang basin is largely divided into three stages ; 1) the Tertiary fault activity and formation of fracture zone, 2) development of erosional basin, 3) local crustal movements and development of fault-related topography. It is assumed that alluvial fans, deflected channel and stream piracy were formed by local tectonic movements related to faultings during the Quaternary.

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Acknowledgement

본 연구는 행정안전부 한반도 단층구조선의 조사 및 평가기술 개발 사업의 연구 지원(2017-MOIS31-006)에 의해 수행되었습니다.