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|a Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites |h [electronic resource]. |
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|a [S.l.] : |b Elsevier, |c 1998. |
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|a Earth and Planetary Sciences Letters Volume 163. |
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|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. |
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|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. |
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|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. |
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|t Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15061978/00001 |y Click here for full text |
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|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 |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/06/19/78/00001/FI15061978thm.jpg |