Seismicity and tectonics around the northern Antarctic Peninsula from King Sejong station data SCIE SCOPUS
DC Field | Value | Language |
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dc.contributor.author | Lee, DK | - |
dc.contributor.author | Jin, YK | - |
dc.contributor.author | Kim, Y | - |
dc.contributor.author | Nam, SH | - |
dc.date.accessioned | 2020-04-21T08:40:17Z | - |
dc.date.available | 2020-04-21T08:40:17Z | - |
dc.date.created | 2020-01-28 | - |
dc.date.issued | 2000-06 | - |
dc.identifier.issn | 0954-1020 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/6058 | - |
dc.description.abstract | Local earthquakes recorded at the King Sejong station (62 degrees 13'31"S, 58 degrees 17'07"W) from 1995-96 have been analysed to study the seismicity and tectonics around the northern Antarctic Peninsula. The nature of shallow-focused normal fault earthquakes along the South Shetland Platform is still unclear. Dominant normal fault earthquakes and minor strike-slip earthquakes in the Eastern Bransfield Basin suggest 1) ongoing extension, and 2) transtensional stress transmitted from the Antarctic-Scotia transform boundaries, the South Scotia Ridge and the Shackleton Fracture Zone. A lack of seismicity in the Central Bransfield Basin supports that active seismicity in the Eastern Bransfield Basin is not a result of subduction along the South Shetland Trench. Shallow focused earthquakes have been observed along the NW-SE trending gravity low line between the Central and the Eastern Bransfield Basins that approximately coincides with the landward projection of a fracture zone in the former Phoenix Plate. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | CAMBRIDGE UNIV PRESS | - |
dc.subject | WEST ANTARCTICA | - |
dc.subject | EVENT DETECTION | - |
dc.subject | SCOTIA SEA | - |
dc.title | Seismicity and tectonics around the northern Antarctic Peninsula from King Sejong station data | - |
dc.type | Article | - |
dc.citation.endPage | 204 | - |
dc.citation.startPage | 196 | - |
dc.citation.title | ANTARCTIC SCIENCE | - |
dc.citation.volume | 12 | - |
dc.citation.number | 2 | - |
dc.identifier.bibliographicCitation | ANTARCTIC SCIENCE, v.12, no.2, pp.196 - 204 | - |
dc.identifier.doi | 10.1017/S0954102000000250 | - |
dc.identifier.scopusid | 2-s2.0-0034213484 | - |
dc.identifier.wosid | 000087775400010 | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.subject.keywordPlus | WEST ANTARCTICA | - |
dc.subject.keywordPlus | EVENT DETECTION | - |
dc.subject.keywordPlus | SCOTIA SEA | - |
dc.subject.keywordAuthor | earthquakes | - |
dc.subject.keywordAuthor | King Sejong station | - |
dc.subject.keywordAuthor | northern Antarctic Peninsula | - |
dc.subject.keywordAuthor | seismicity | - |
dc.subject.keywordAuthor | tectonics | - |
dc.relation.journalWebOfScienceCategory | Environmental Sciences | - |
dc.relation.journalWebOfScienceCategory | Geography, Physical | - |
dc.relation.journalWebOfScienceCategory | Geosciences, Multidisciplinary | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Environmental Sciences & Ecology | - |
dc.relation.journalResearchArea | Physical Geography | - |
dc.relation.journalResearchArea | Geology | - |