Tectonics of the Oppdal area, central Norway
作者:
AllanG. Krill,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1980)
卷期:
Volume 102,
issue 4
页码: 523-530
ISSN:0016-786X
年代: 1980
DOI:10.1080/11035898009454505
出版商: Taylor & Francis Group
关键词: Areal geology;tectonics;lithostratigraphy;thrust faults;nappes;recumbent folds;augen gneiss;dolerite;dykes;metamorphic rocks;Caledonian Orogeny;Trondheim Nappe Complex;Western Gneiss Region;Proterozoic;Lower Paleozoic;Oppdal;southern Sør Trøndel
数据来源: Taylor
摘要:
In the Oppdal area, a sequence of Caledonian thrust nappes was metamorphosed, recumbently folded, and refolded during the Caledonian orogeny. The well known Oppdal augen gneisses are Proterozoic rocks belonging to a single nappe unit in the tectonostratigraphy. Another distinctive nappe unit was formed from feldspathic sandstone, intruded in late Proterozoic time by pre-tectonic dolerite dikes. Despite the new thrust interpretations, the early concept of ductile infrastructurel deformation below a more rigid superstructure may still be accurate here in one of Wegmann's type localities of theStockwerktectonic model.
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