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沖積面에서 본 後氷期以來의 汀線變化 : The Changes of Shore Line after Post-Glaicial Age in Central Area of Korea

DC Field Value Language
dc.contributor.author金相昊-
dc.date.accessioned2014-01-20T01:27:00Z-
dc.date.available2014-01-20T01:27:00Z-
dc.date.issued1977-12-
dc.identifier.citation지리학논총, Vol.4, pp. 1-5-
dc.identifier.issn1226-5888-
dc.identifier.urihttps://hdl.handle.net/10371/89423-
dc.description.abstractThe changes of shore line after post-glacial age was analysed through Holocene deposit in central area of Korea. The approximate limsit of share line raised in Post-glacial period has a height of 6pm from present sea level in west coast as well as in east coast of central Korea.

Kyong-gee-man transgression, which would be correlated with Dunkearque transgression, in also recognized in the same coast.
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dc.language.isoko-
dc.publisher서울대학교 국토문제연구소-
dc.title沖積面에서 본 後氷期以來의 汀線變化-
dc.title.alternativeThe Changes of Shore Line after Post-Glaicial Age in Central Area of Korea-
dc.typeSNU Journal-
dc.contributor.AlternativeAuthorKim, Sang Ho-
dc.citation.journaltitle지리학논총(Journal of Geography)-
dc.citation.endpage5-
dc.citation.pages1-5-
dc.citation.startpage1-
dc.citation.volume4-
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