A1 Refereed original research article in a scientific journal

Zircon dating of the basalt and felsic dyke in Haveri, SW Finland




AuthorsKara Jaakko, Väisänen Markku, O'Brien Hugh

PublisherGeological Society of Finland

Publication year2022

JournalBulletin of the Geological Society of Finland

Volume94

Issue2

First page 109

Last page118

eISSN1799-4632

DOIhttps://doi.org/10.17741/bgsf/94.2.001

Web address http://dx.doi.org/10.17741%2Fbgsf%2F94.2.001

Self-archived copy’s web addresshttps://research.utu.fi/converis/portal/detail/Publication/177978350


Abstract

The E-MORB type Haveri basalt differs from the volcanic arc type rocks in the Tampere
belt showing no subduction signature. It is considered to have formed in a marginal
basin prior to the volcanic arc. We present here zircon U-Pb dating on two samples. The
basalt and the felsic dyke yielded 207Pb/206Pb ages of 1902 ± 5 Ma and 1891 ± 2 Ma,
respectively, interpreted as crystallisation ages. The basalt also contains older 1.98 Ga
grains while the felsic dyke contains older 1.92 Ga, 1.94 Ga, 1.98 Ga and 2.0 Ga grains,
which are inferred as inherited. The age dating of E-MORB type basalts can be used to
identify the extensional episodes of the accretionary Svecofennian orogeny.


Downloadable publication

This is an electronic reprint of the original article.
This reprint may differ from the original in pagination and typographic detail. Please cite the original version.





Last updated on 2024-26-11 at 12:50