남극반도 스미스섬 부근 대륙주변부의 탄성파 구조

Seismic Structures of the Continental Margin around Smith Island, antarctic Peninsula

  • 진영근 (한국해양연구원 부설 극지연구소/경북대학교) ;
  • 남상헌 (한국해양연구원 부설 극지연구소) ;
  • 이주한 (한국해양연구원 부설 극지연구소) ;
  • 홍종국 (한국해양연구원 부설 극지연구소) ;
  • 이덕기 (기상청) ;
  • 이종익 (한국해양연구원 부설 극지연구소)
  • 발행 : 20060000

초록

남극반도 북부 남셰틀랜드군도 남서부에 위치한 스미스섬 부근 대륙주변부에서 작성된 탄성파 단면도를 분석하여 이 지역의 퇴적층의 분포, 퇴적작용, 대륙붕 형성과정 및 지체구조 발달사를 고찰하였다. 연구지역은 히어로 파쇄대의 대륙쪽 연장선에 위치한 스미스섬을 경계로 지체구조적으로 매우 상이한 두 지역으로 나눌 수 있다. 스미스섬의 남서쪽 지역은 확장중심-해구이 충돌 결과로 형성된 비활동성 대륙주변부가 전개되며, 북동쪽 지역은확장중심과 해구의 구조가 해양에 남아 있는 활동성 대륙주변부가 발달해 있다. 전체적으로 스미스섬을 경계로 북동쪽 지역에서는 두꺼운 퇴적층을 가진 대륙붕 퇴적층지역과 전호분지가 발달되어 있으며, 상대적으로 넓은 대륙사면과 뚜렷한 형태의 해구를 볼 수 있다. 남서쪽 지역은 가파르고 좁은 대륙사면과 국부적으로 형성된 대륙붕분지들이 특징적으로 나타난다. 또한 남서쪽 지역에는 이미 섭입된 확장중심의 열적효과(thermal effect)의 결과로 형성된 것으로 해석되는 기반암 상승부가 대륙붕의 중간부에 잘 발달되어 있다. 기반암 상승부는 스미스섬의 북동쪽을 연장되어 히어로파쇄대를 따라 형성된 경계부가 뚜렷한 지체구조 경계를 형성하지는 않는 것으로 해석된다.

Using seismic profiles obtained in the Antarctic Peninsula continental margin around Smith Island located at the southwestern end of the South Shetland Islands, we investigated sediments distribution, sedimentation, continental shelf formation, and tectonic evolution history. The study area is a very unique area that has two tectonic provinces with a tectonic boundary near Smith Island just the landward projection of the Hero Fracture Zone (HFZ). To the southwest of the Island, the margin became inactive margin after the collision of the ridge crest of the Antarctic-Phoenix ridge and trench, whereas to the northeast the margin is still apparently active margin with the spreading center and trench morphology in the sea. Generally the northeastern margin has the shelf sedimentary basins wth thick sedimentary layers, well-developed forearc basin, broad continental slope and distinct trench morphology, and the southwestern margin is characterized by steep and narrow continental slope and localized shelf basins. the mid-shelf basement high structures are distinct in the southwestern margin, which are thought to be formed by thermal effect caused by the subducted spreading centers. The high is observed in the area just northeast of the Island, implying that the tectonic boundary along the landward projection of the HFZ is not sharply defined.

키워드

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