Altimetry-Derived Gravity Predictions of Bathymetry by the Gravity-Geologic Method
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Ralph | - |
dc.contributor.author | Daniel | - |
dc.contributor.author | Kim, Jeong Woo | - |
dc.contributor.author | Lee, Bang Yong | - |
dc.contributor.author | Doh, Seong-Jae | - |
dc.coverage.spatial | Drake Passage | - |
dc.coverage.spatial | Antarctica | - |
dc.date.accessioned | 2018-03-20T13:39:59Z | - |
dc.date.available | 2018-03-20T13:39:59Z | - |
dc.date.issued | 2010 | - |
dc.identifier.uri | https://repository.kopri.re.kr/handle/201206/6070 | - |
dc.description.abstract | The gravity-geologic method (GGM) was implemented for 20 by 20 bathymetric eterminations in a 1.6o longitudeby-1.0o latitude region centered on the eastern end of the Shackleton Fracture Zone in the Drake Passage, Antarctica. | - |
dc.language | English | - |
dc.publisher | Springer Basel AG | - |
dc.subject | Geochemistry & Geophysics | - |
dc.title | Altimetry-Derived Gravity Predictions of Bathymetry by the Gravity-Geologic Method | - |
dc.title.alternative | 중력 지질학적인 방법에 의한 수심측량자료의 고도유래 중력 예측 | - |
dc.type | Article | - |
dc.identifier.bibliographicCitation | Ralph, et al. 2010. "Altimetry-Derived Gravity Predictions of Bathymetry by the Gravity-Geologic Method". <em>Pure and Applied Geophysics</em>, 168(5): 815-826. | - |
dc.citation.title | Pure and Applied Geophysics | - |
dc.citation.volume | 168 | - |
dc.citation.number | 5 | - |
dc.identifier.doi | 10.1007/s00024-010-0170-5 | - |
dc.citation.startPage | 815 | - |
dc.citation.endPage | 826 | - |
dc.description.articleClassification | SCI | - |
dc.description.jcrRate | JCR 2008:65.625 | - |
dc.subject.keyword | Antarctica | - |
dc.subject.keyword | Bathymetry prediction | - |
dc.subject.keyword | Drake Passage | - |
dc.subject.keyword | altimetry derived gravity anom | - |
dc.subject.keyword | gravity geologic method | - |
dc.identifier.localId | 2010-0077 | - |
dc.identifier.scopusid | 2-s2.0-79959770711 | - |
dc.identifier.wosid | 000289805200005 | - |
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