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160206s1984 xx |||||o 00| ||eng c |
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|a (DE-627)JST09890499X
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|a (JST)43317028
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|a DE-627
|b ger
|c DE-627
|e rakwb
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|a eng
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|a Mörner, Nils-Axel
|e verfasserin
|4 aut
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|a Differential Holocene Sea Level Changes Over the Globe: Evidence for Glacial Eustasy, Geoidal Eustasy, and Crustal Movements
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|c 1984
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|a Text
|b txt
|2 rdacontent
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|a Computermedien
|b c
|2 rdamedia
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|a Online-Ressource
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|2 rdacarrier
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|a The old theory of eustasy implied that the eustatic ocean level was displaced up and down smultaneously and equally over the globe. Due to the geoid deformation, however, two eustatic levels are never quite parallel. The present paper deals with the complexity of variables and the Holocene global observational records.
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|a © 1984 Van Nostrand Reihold Company
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| 650 |
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4 |
|a Physical sciences
|x Metrology
|x Altimetry
|x Altitude
|x Sea level
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| 650 |
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4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Geodesy
|x Geoids
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| 650 |
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4 |
|a Physical sciences
|x Earth sciences
|x Geology
|x Glaciology
|x Glacial landforms
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| 650 |
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4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Bodies of water
|x Seas
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| 650 |
|
4 |
|a Physical sciences
|x Earth sciences
|x Geology
|x Geologic processes
|x Isostasy
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| 650 |
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4 |
|a Behavioral sciences
|x Human behavior
|x Transgression
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| 650 |
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4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Bodies of water
|x Oceans
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| 650 |
|
4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Land
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| 650 |
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4 |
|a Physical sciences
|x Physics
|x Mechanics
|x Continuum mechanics
|x Deformation
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| 650 |
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4 |
|a Physical sciences
|x Earth sciences
|x Geology
|x Tectonics
|x TECHNICAL COMMUNICATIONS
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| 655 |
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4 |
|a research-article
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| 773 |
0 |
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|i Enthalten in
|t Litoralia
|d Van Nostrand Reihold Company Inc., 1984
|g 1(1984), 1, Seite 83-86
|w (DE-627)JST098904884
|x 24706035
|7 nnas
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| 773 |
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|g volume:1
|g year:1984
|g number:1
|g pages:83-86
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|u https://www.jstor.org/stable/43317028
|3 Volltext
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|d 1
|j 1984
|e 1
|h 83-86
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