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pro vyhledávání: '"Christer Hoel"'
Publikováno v:
Journal of Geodynamics. 44:96-128
The Younger Dryas (YD) maximum highstand shoreline in SW Norway has traditionally been considered as being slightly concave, gradually steepening in the direction of uplift. This phenomenon is attributed to geoidal and isostatic effects near the form
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dc4312adfe2e56deecfbb9f1ac7f39f
https://doi.org/10.1016/j.jog.2007.01.001
https://doi.org/10.1016/j.jog.2007.01.001
