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001        FI15061978_00001
005        20160201105015.0
006        m^^^^^o^^d^^^^^^^^
007        cr^^n^---ma^mp
008        150714n^^^^^^^^xx^||||^o^^^^^|||^u^eng^d
245 00 |a Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites |h [electronic resource].
260        |a [S.l.] : |b Elsevier, |c 1998.
490        |a Earth and Planetary Sciences Letters Volume 163.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a The eustatic component of relative sea-level change provides a measure of the amount of ice transferred between the continents and oceans during glacial cycles. This has been quantified for the period since the Last Glacial Maximum by correcting observed sea-level change for the glacio-hydro-isostatic contributions using realistic ice distribution and earth models.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650    0 |a Climate Change.
650    0 |a Sea Level Rise.
650    0 |a Glaciology.
720 1    |a Fleming, Kevin.
720 1    |a Johnston, Paul.
720 1    |a Zwartz, Dan.
720 1    |a Yokoyama, Yusuke.
720 1    |a Lambeck, Kurt.
720 1    |a Chappell, John.
773 0    |t Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15061978/00001 |y Click here for full text
856 42 |3 Host material |u http://www.sciencedirect.com/science/article/pii/S0012821X98001988 |y Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/19/78/00001/FI15061978thm.jpg
997        |a Sea Level Rise


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