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Shear zones and structural analysis of the Loimaa area, SW Finland




AuthorsIiro Pitkälä, Jaakko Kara, Tuomas Leskelä, Pietari Skyttä, Markku Väisänen, Hanna Leväniemi, Janne Hokka, Markku Tiainen, Yann Lahaye

EditorsIlmo Kukkonen, Suvi Heinonen, Hanna Silvennoinen, Fredrik Karell, Elena Kozlovskaya, Arto Luttinen, Kaisa Nikkilä, Vesa Nykänen, Markku Poutanen, Pietari Skyttä, Eija Tanskanen, Timo Tiira and Kati Oinonen

Conference nameLITHOSPHERE

Publication year2018

Book title LITHOSPHERE 2018: TENTH SYMPOSIUM ON STRUCTURE, COMPOSITION AND EVOLUTION OF THE LITHOSPHERE: PROGRAMME AND EXTENDED ABSTRACTS

Series titleREPORT

Number in series67

First page 91

Last page94

ISBN978-952-10-9594-8

eISBN978-952-10-9595-5

Web address http://www.seismo.helsinki.fi/ilp/lito2018/Lito2018_Abstract_Volume_color.pdf

Self-archived copy’s web addresshttps://research.utu.fi/converis/portal/detail/Publication/37200930


Abstract

Shear zones of various ages and orientations are common in Southern Finland. In the study area, E-W and N-S trending shear zones are the dominant structural feature. Mylonitic foliations were identified from the most intensely sheared rocks. Ductile shearing has mainly been of dip-slip type. Structural mapping revealed several larger map-scale folds, which appear to be relatively continuous across the study area from SE to NW. In the central area, folding interfered with the shear zones causing a complex crustal structure such as associated with the Uunimäki mineralization. Aeromagnetic and lithological maps, field observations, stereographic projections and oriented thin sections were used to determine the structural features of the study area.


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