COURSE AND ORIGIN OF THE FENNOSCANDIAN UPLIFT - THE CASE FOR 2 SEPARATE MECHANISMS

被引：9
作者：
MORNER, NA
机构：
[1] Paleogeophysics & Geodynamics, Stockholm University, Stockholm
来源：
TERRA NOVA | 1991年 / 3卷 / 04期
关键词：
D O I：
10.1111/j.1365-3121.1991.tb00170.x
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
The classical glacial isostatic uplift paradigm of Fennoscandia is in need of a thorough revision as to its course and origin. The total uplift amounts to 830 m (not 300 m). The centre of uplift started to rise 13,000 BP (not 9300 BP). The uplift appears to be composed of two separate mechanisms; one true glacial isostatic rebound, and one linear uplift factor possibly representing a phase boundary adjustment. Calculations and modelling must treat these two factors independently (which has not been the case).
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页码：408 / 413
页数：6
相关论文
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