Depositional features of co-genetic turbidite-debrite beds and possible mechanisms for their formation in distal mass-flow lobes beyond the base-of-slope, Ulleung Basin, East Sea

DC Field Value Language
dc.contributor.author 이상훈 -
dc.contributor.author 정우열 -
dc.contributor.author 박장준 -
dc.contributor.author Joan M. Gardner -
dc.contributor.author 박준용 -
dc.contributor.author 이희준 -
dc.contributor.author 김진경 -
dc.contributor.author 이수환 -
dc.date.accessioned 2020-07-16T11:32:02Z -
dc.date.available 2020-07-16T11:32:02Z -
dc.date.created 2020-02-11 -
dc.date.issued 2012-10-24 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/27501 -
dc.description.abstract A detailed analysis of the MR1 (11−12 kHz) sonar images, chirp (2−7 kHz) profiles,core sediments and 14C ages from the latest Quaternary mass-flow lobes on the deep(>2,100 m water depth) basin plain of the western Ulleung Basin reveals various depositional processes of mass flows in the distal setting beyond the base-of-slope and changes in slope-failure style. Eight mass-flow lobes are present in the basin plain, ca. 30−60 km beyond the base-of-slope, and were generally deposited retrogressively. Lobes 1−4 (distal lobes) are longer (>27 km) and wider (15−25 km) than lobes 5−8 (proximal lobes) having the length of 8.8−31.5 km and the width of 1.2−12 km. Lobes 1 and 2 consist dominantly of the muddier mass-flow deposits deposited between 19.5 and 20.0 cal. ka B.P. after the Last Glacial Maximum. The relatively huge masses with the high content of muds failed on the muddy upper slopes, deeper than 350−400 m water depth. On other hand, the sandier, smaller lobes 6 and 7 were deposited between 16.5 and 17 cal. ka B.P., probably by sediment failures on the sandy uppermost slope, shallower than 350−400 m water depth. Lobe 1 consists of a lower sandy-mud turbidite grading upward into an upper mud-matrix debrite having small, rounded mud clasts. In contrast, the mass-flow bed of lobe 6 is characterized by a gradual upward change from a lower clay-posin reveals various depositional processes of mass flows in the distal setting beyond the base-of-slope and changes in slope-failure style. Eight mass-flow lobes are present in the basin plain, ca. 30−60 km beyond the base-of-slope, and were generally deposited retrogressively. Lobes 1−4 (distal lobes) are longer (>27 km) and wider (15−25 km) than lobes 5−8 (proximal lobes) having the length of 8.8−31.5 km and the width of 1.2−12 km. Lobes 1 and 2 consist dominantly of the muddier mass-flow deposits deposited between 19.5 and 20.0 -
dc.description.uri 2 -
dc.language English -
dc.publisher 대한지질학회 -
dc.relation.isPartOf 2012추계지질과학연합학술대회 -
dc.title Depositional features of co-genetic turbidite-debrite beds and possible mechanisms for their formation in distal mass-flow lobes beyond the base-of-slope, Ulleung Basin, East Sea -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 13 -
dc.citation.startPage 13 -
dc.citation.title 2012추계지질과학연합학술대회 -
dc.contributor.alternativeName 이상훈 -
dc.contributor.alternativeName 박준용 -
dc.contributor.alternativeName 이희준 -
dc.contributor.alternativeName 김진경 -
dc.contributor.alternativeName 이수환 -
dc.identifier.bibliographicCitation 2012추계지질과학연합학술대회, pp.13 -
dc.description.journalClass 2 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Climate Response & Ecosystem Research Department > 2. Conference Papers
Files in This Item:
There are no files associated with this item.

qrcode

Items in ScienceWatch@KIOST are protected by copyright, with all rights reserved, unless otherwise indicated.

Browse