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PRELIMINARY RESULTS OF SEISMIC SURVEY IN THE CENTRAL BRANSFIELD STRAIT, ANTARCTIC PENINSULA
https://doi.org/10.15094/00002830
https://doi.org/10.15094/0000283030e5a02f-1225-4f23-ae43-101b77850e08
名前 / ファイル | ライセンス | アクション |
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KJ00002409877 (1.0 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1996-09-01 | |||||
タイトル | ||||||
タイトル | PRELIMINARY RESULTS OF SEISMIC SURVEY IN THE CENTRAL BRANSFIELD STRAIT, ANTARCTIC PENINSULA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | the central Bransfield Strait | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | multichannel seismic survey | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | transform fault | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | basinward-dipping reflectors | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002830 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | PRELIMINARY RESULTS OF SEISMIC SURVEY IN THE CENTRAL BRANSFIELD STRAIT, ANTARCTIC PENINSULA | |||||
著者名よみ |
/
× /× / |
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著者名(英) |
JIN, Young Keun
× JIN, Young Keun× KIM, Yeadong× KIM, Hyoung-Soo× NAM, Sang Heon |
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著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Multichannel seismic profiles in the central Bransfield Strait show structural variation mainly controlled by transform faults across the strait. Near King George Island, large displacement of the spreading axis, discontinuity and different style of the faults, intense deformation of the basement, and abrupt change in the morphology of the basin are indicative of the presence of a large fault zone. On the basis of the fault map, the central Bransfield Strait can be divided into three segments. Transform faults, including the large fault zone, form the boundaries of segments. The basinward-dipping reflectors concentrated in the central segment suggest that initial rifting activity was relatively strong in this region. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 9, p. 141-149, 発行日 1996-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |