Late Proterozoic tectonic events in southern Finland, constrained by Ar-40/Ar-39 incremental heating and single spot fusion experiments on K-feldspars.

M. Heeremans; J.R. Wijbrans

doi:10.1046/j.1365-3121.1999.00250.x

Late Proterozoic tectonic events in southern Finland, constrained by Ar-40/Ar-39 incremental heating and single spot fusion experiments on K-feldspars.

M. Heeremans, J.R. Wijbrans

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

The post-Svecofennian tectonic development of southern Finland is controlled by intrusion of rapakivi granites (and associated rocks), reactivation of Svecofennian wrench zones, formation of sedimentary basins and successive intrusion of olivine dolerite dykes and sills. Relative age determinations have revealed that fault reactivation acted before, simultaneously and after intrusion of the rapakivi granites. Results of

Original language	English
Pages (from-to)	216-222
Journal	Terra Nova
Volume	11
Issue number	5
DOIs	https://doi.org/10.1046/j.1365-3121.1999.00250.x
Publication status	Published - 1999

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10.1046/j.1365-3121.1999.00250.x

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title = "Late Proterozoic tectonic events in southern Finland, constrained by Ar-40/Ar-39 incremental heating and single spot fusion experiments on K-feldspars.",

abstract = "The post-Svecofennian tectonic development of southern Finland is controlled by intrusion of rapakivi granites (and associated rocks), reactivation of Svecofennian wrench zones, formation of sedimentary basins and successive intrusion of olivine dolerite dykes and sills. Relative age determinations have revealed that fault reactivation acted before, simultaneously and after intrusion of the rapakivi granites. Results of",

author = "M. Heeremans and J.R. Wijbrans",

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AU - Wijbrans, J.R.

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Y1 - 1999

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AB - The post-Svecofennian tectonic development of southern Finland is controlled by intrusion of rapakivi granites (and associated rocks), reactivation of Svecofennian wrench zones, formation of sedimentary basins and successive intrusion of olivine dolerite dykes and sills. Relative age determinations have revealed that fault reactivation acted before, simultaneously and after intrusion of the rapakivi granites. Results of

U2 - 10.1046/j.1365-3121.1999.00250.x

DO - 10.1046/j.1365-3121.1999.00250.x

M3 - Article

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Late Proterozoic tectonic events in southern Finland, constrained by Ar-40/Ar-39 incremental heating and single spot fusion experiments on K-feldspars.

Abstract

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