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A case study of lateral spreading: the Precambrian Svecofennian Orogen

By
Annakaisa Korja
Annakaisa Korja
Institute of Seismology, POB 68, FI-00014
University of Helsinki
,
Finland
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Paula Kosunen
Paula Kosunen
Institute of Seismology, POB 68, FI-00014
University of Helsinki
,
Finland
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Pekka Heikkinen
Pekka Heikkinen
Institute of Seismology, POB 68, FI-00014
University of Helsinki
,
Finland
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Published:
January 01, 2009

Abstract

We have studied the crustal structures of the Palaeoproterozoic Svecofennian (c. 1.9 Ga) Orogeny with the help of large scale seismic reflection surveys (FIRE 1–3), preliminary structural field work and geological and geophysical databases. The central part of the orogen is occupied by the Central Finland Granitoid Complex, which comprises two suites of granitoid rocks and associated mafic and volcanic rocks. The complex and the surrounding supracrustal belts are cut and deformed by numerous shear zones and faults; here divided into six groups. The most prominent reflections are usually shear zones or faults on outcrops. The granitoid complex is interpreted as a deep, lower-level section of an old core complex, where the younger granitoid intrusions form the basins and older granitoid intrusions and associated volcanic rocks form the horsts. The upper–middle crust detachment zone is exposed at the northeastern edge of the complex and middle crust is exposed in the migmatitic domes at northern and western margins.

The seismic reflection sections display a frozen image of orogenic thickening and lateral spreading. The decoupling of the upper, middle and lower crust during spreading resulted in the formation of layered superstructure–infrastructure of the crust.

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Contents

Geological Society, London, Special Publications

Extending a Continent: Architecture, Rheology and Heat Budget

U. Ring
U. Ring
University of Canterbury, New Zealand
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B. Wernicke
B. Wernicke
California Institute of Technology, USA
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Geological Society of London
Volume
321
ISBN electronic:
9781862395695
Publication date:
January 01, 2009

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