Mylonites and pseudotachylites associated with thrusting of the Köli Nappes, Tännforsfältet, central Swedish Caledonides
作者:
Monica Beckholmen,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1982)
卷期:
Volume 104,
issue 1
页码: 23-32
ISSN:0016-786X
年代: 1982
DOI:10.1080/11035898209454532
出版商: Taylor & Francis Group
关键词: Mylonite zones;pseudotachylite;thrust;ductile;plastically;brittle;brecciation;cataclastic;stress;discontinuous deformation;shock wave;Caledonides;Köli Nappes;Tännforsfältet;tectonic units;garbenschiefer;calcareous phyllite;Gevsjön Form
数据来源: Taylor
摘要:
The Gevsjön Formation (calcareous phyllite — garbenschiefer) of the Tännforsfältet Köli is divided into three tectonic units, separated by two important mylonite zones. These mylonite zones exhibit an earlier ductile phase of deformation and a later brittle phase with brecciation of the mylonitic foliation. Associated with this brecciation pseudotachylites have been recognized at four localities. A fifth locality is so far not directly related to any mylonite zone, but occurs close below the upper mylonite zone. The change from mylonite formation (ductile deformation) to the development of breccias and pseudotachylites represents a change in physical conditions during translation of the nappes. Early movement occurred at higher and the later movement at lower temperatures, implying that the thrusting involved progressive translation of the Köli Nappes to higher structural levels.
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