The Precambrian development of southern Sweden
作者:
Roland Gorbatschev,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1980)
卷期:
Volume 102,
issue 2
页码: 129-136
ISSN:0016-786X
年代: 1980
DOI:10.1080/11035898009450890
出版商: Taylor & Francis Group
关键词: Areal geology Baltic Shield;Småland-Vämland Belt;Protogine Zone;Mylonite Zone;Svecofennian;Svecokarelian;Gothian;Sveconorvegian;Dalslandian;Grenvillian;Proterozoic;southern Sweden;new tectonic unit;N5500 N6400 E1900 E1300
数据来源: Taylor
摘要:
The Precambrian of southern Sweden represents a gradual accretion of the Baltic Shield. The Svecofennian region in the east was stabilized by about 1750 Ma. In the west, an orogenic event between ca. 1600 and 1700 Ma added new continental crust to the shield, possibly also reworking a marginal segment of the Svecofennian. A continuous belt of granites and porphyries marks the boundary of the south-western orogen with the stable Svecofennian region. The subsequent development of southern Sweden was essentially ensialic, periods of granite intrusion and metamorphism interrupting anorogenic developments. In a final culmination of activity around 900–1100 Ma, southern Sweden played the role of a crustal segment marginal to the Grenvillian orogen.
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