지원사업
학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
커뮤니티
연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
논문 기본 정보
- 자료유형
- 학술저널
- 저자정보
- 발행연도
- 2006.1
- 수록면
- 189 - 197 (9page)
이용수
초록· 키워드
오류제보하기
The Korea Plateau is a continental fragment rifted and partially segmented from the Korean Peninsulaat the initial stage of the opening of the East Sea (Japan Sea). We interpreted marine seismic profiles from the South Korea Plateau in conjunction with swath bathymetric to investigate processes of con-tjnental rifting and separation of the southwestern Japan Arc. The SouU-i Korea Plateau preserves funda-mental elements of rift architecture comprising a seaward succession of a rift basin and an uplifted rift flank passing into the slope, typical of a passive continental margin. Two distinguished rift basins (Onnuri and Bandal Basins) in the South Korea Plateau are bounded by major synthetic and smaller antithetic faults, creating wide and symmetric profiles. The large-offset border fault zones of these basins have convex dip slopes and demonstrate a zig-zag arrangement along strike. Rifting was primarily controlled by normal faulting resulting from extension orthogonal to the inferred line of breakup along the base ofthe slope rather U-ian strike-slip deformation. Two extension direcdons for rifdng are recog-nized; U-ie Onnuri Basin was rifted in U-ie EW direction; U-ie Bandal Basin in U-ie EW and NW-SE directions, suggesting two rift stages. We interpret that the E-W direction represents initial rifting at the inner margin; while the Japan Basin widened, rifting propagated repeatedly from the Japan Basin to the southeast toward the Korean margin but could not penetrate the strong continental lithosphere of the Korean Shield and changed direction to the south, resulting in E-W extension to create the rift basins at the Korean margin. The Hupo Basin to the south of the Korea Plateau is estimated to have formed in this process. The NW-SE direction probably represents the direction of rifting orthogonal to the inferred line of breakup along the base of the slope of the South Korea Plateau; after breakup the southwestern Japan Arc separated in the SE direction, indicating a response to tensional tectonics associated with the subduction of the Pacific Plate in the NE direction. We suggest that structural evolution of the eastern Korean margin can be explained by the processes occurring at the passive continental margin.
목차
등록된 정보가 없습니다.
참고문헌 (0)
참고문헌 신청함께 읽어보면 좋을 논문
논문 유사도에 따라 DBpia 가 추천하는 논문입니다. 함께 보면 좋을 연관 논문을 확인해보세요!
-
Evolution of the eastern margin of Korea: constraints on the opening of the East Sea (Japan Sea)
한국지구물리탐사학회 심포지움
2007 .01
-
한국 동쪽 대륙주변부의 구조적 진화와 동해의 형성
자원환경지질
2006 .01
-
Cretaceous syn-rift to post-rift subsidence history of the Naturaliste Plateau, offshore southwest Australia (IODP Site U1513)
대한지질학회 학술대회
2019 .10
-
Crustal structure of the continental margin of Korea in the East Sea (Japan Sea) from deep seismic sounding data : evidence for rifting affected by the hotter than normal mantle
대한지질학회 학술대회
2002 .10
-
The rift Caves in Japan
동굴
1997 .01
-
A study on geomorphological sketch of middle part of Korea
동굴
2007 .01
-
Surface wave tomography in the Main Ethiopian Rift using ambient seismic noise
대한지질학회 학술대회
2010 .10
-
Pressure and Temperature evolution of upper mantle under the Rio Grande rift
대한지질학회 학술대회
2003 .10
-
Application of heavy minerals as rift-related depositional system criteria in alluvial to fluvial environment: As an example from the Cheju Basin (NE East China Sea) Dragon-1 Well, Korea
한국석유지질학회 학술발표회
1998 .01
-
Tectonic evolution of the western Kunsan Basin, Yellow Sea, offshore Korea
지질학회지
2005 .06
-
The Structural and Stratigraphic Evolution of Lake Tanganyika
자원환경지질
1997 .01
-
The Neoproterozoic transition from arc to rift tectonic setting in the Hongseong area, the southwestern part of Gyeonggi block in South Korea and its meaning to the tectonic evolution of Northeast Asia
대한지질학회 학술대회
2008 .10
-
남해 제주분지 해역의 퇴적환경 및 지질구조 예비 해석
지구물리와 물리탐사
2004 .01
-
Seismic characteristics of the continental margin around Korea and Japan
대한지질학회 학술대회
2009 .10
-
Structural Evolution of the Southern Margin of the Ulleung Basin, East Sea (Japan Sea)
대한지질학회 학술대회
2007 .10
-
Hydrothermal activities in the Fonualei Spreading and Rift Center (FRSC) in the Lau basin, southwestern Pacific : Preliminary data
대한지질학회 학술대회
2006 .10
-
Physicochemical heterogeneity of upper mantle inferred from deformation microstructures beneath the Rio Grande rift
대한지질학회 학술대회
2013 .10
-
Deformation microstructures of spinel peridotite from the Rio Grande rift, New Mexico
대한지질학회 학술대회
2009 .10
-
Hydroacoustic study of an ultra-slow continental rifting in the Bransfield Strait, Antarctica
대한지질학회 학술대회
2008 .10
-
Upper mantle velocity structure beneath the Kenya Rift using teleseismic P-wave tomography
한국지구물리탐사학회 학술대회
2009 .01
이 논문의 저자 정보
최근 본 자료
댓글(0)
0