Estimation of postglacial sea levels from fennosgandian data
作者： H. R. Thompson
DOI: 10.1080/00288306.1964.10420183
关键词: Sea level 、 Geology 、 Post-glacial rebound 、 Geodesy
摘要: Abstract If we let the unknown value of sea level, j thousand years ago, be x and strandline level at locality i for time y ij (both related to present level), then isostatic rebound is — , assumption that amounts different localities are proportional each other implies fd_361 values j, where f proportionality constants 1 2 etc., k similar points time.
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