Note on estimates of the glacial-isostatic decay spectrum for Fennoscandia

被引：8
|
作者：
Wolf, D [1 ]
机构：
[1] UNIV MUNSTER,INST PLANETOL,D-48149 MUNSTER,GERMANY
来源：
GEOPHYSICAL JOURNAL INTERNATIONAL | 1996年 / 127卷 / 03期
关键词：
Fennoscandia; glacial rebound; isostasy; mantle viscosity; sea level;
D O I：
10.1111/j.1365-246X.1996.tb04059.x
中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
For more than 30 years, Sauramo's (1958) shoreline diagram of the Fennoscandian uplift has been used in geophysical studies for estimates of the glacial-isostatic decay spectrum in order to infer from it the viscosity stratification in the Earth's mantle below Fennoscandia. The intent of the present note is to point out that more recent geological studies suggest that Sauramo's shoreline diagram is an incorrect representation of the Fennoscandian uplift. Geophysical interpretations based on the diagram may therefore require revision.
引用
收藏
页码：801 / 805
页数：5
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