Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland
<p>The southern Finland granites and associated migmatitic rocks have a complex metamorphic history, being affected by multiple events during the ca. 1.88–1.79 Ga Svecofennian orogeny. In this study, the prolonged tectonic evolution of migmatites and associated rocks in southwestern Finland ha...
Saved in:
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-02-01
|
| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/16/97/2025/se-16-97-2025.pdf |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| _version_ | 1823859267547955200 |
|---|---|
| author | J. Engström J. Engström K. Cutts S. Glorie E. Heilimo E. M. Jolis R. M. Michallik |
| author_facet | J. Engström J. Engström K. Cutts S. Glorie E. Heilimo E. M. Jolis R. M. Michallik |
| author_sort | J. Engström |
| collection | DOAJ |
| description | <p>The southern Finland granites and associated migmatitic rocks have a complex metamorphic history, being affected by multiple events during the ca. 1.88–1.79 Ga Svecofennian orogeny. In this study, the prolonged tectonic evolution of migmatites and associated rocks in southwestern Finland has been investigated using the new in situ Lu–Hf method. Results reveal detailed temporal constraints for the tectonic evolution that can be linked to major events in adjacent tectonic blocks in both Finland and Sweden during the Svecofennian orogeny. The metamorphic peak at the Olkiluoto site occurred at 1829 <span class="inline-formula">±</span> 19 Ma based on in situ Lu–Hf dating of garnet. The pressure–temperature (<span class="inline-formula"><i>P</i></span>–<span class="inline-formula"><i>T</i></span>) path for the rocks indicates a prograde evolution, with peak <span class="inline-formula"><i>P</i></span>–<span class="inline-formula"><i>T</i></span> conditions of 3–5 kbar and approximately 700 °C. Younger ages of ca. 1780 Ma obtained using both Lu–Hf and U–Pb systems in apatite inclusions in garnet indicate rapid cooling at 1780 Ma. Based on the metamorphic constraints and obtained ages, we link the Olkiluoto site to the Häme orogenic belt in southern Finland and also support the proposed thermal–tectonic connection with the Ljusdal lithotectonic unit in central Sweden.</p> |
| format | Article |
| id | doaj-art-a0120cff6945455585e6f3e0a60478b6 |
| institution | Kabale University |
| issn | 1869-9510 1869-9529 |
| language | English |
| publishDate | 2025-02-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Solid Earth |
| spelling | doaj-art-a0120cff6945455585e6f3e0a60478b62025-02-11T06:09:16ZengCopernicus PublicationsSolid Earth1869-95101869-95292025-02-01169711710.5194/se-16-97-2025Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern FinlandJ. Engström0J. Engström1K. Cutts2S. Glorie3E. Heilimo4E. M. Jolis5R. M. Michallik6Geological Survey of Finland, P.O. Box 96, 02151 Espoo, FinlandDepartment of Geology and Mineralogy, Åbo Akademi University, Akatemiakatu 1, 20500 Turku, FinlandGeological Survey of Finland, P.O. Box 96, 02151 Espoo, FinlandDepartment of Earth Sciences, University of Adelaide, Adelaide, SA 5005, AustraliaDepartment of Geography and Geology, University of Turku, Akatemiakatu 1, 20500 Turku, FinlandGeological Survey of Finland, P.O. Box 96, 02151 Espoo, FinlandGeological Survey of Finland, P.O. Box 96, 02151 Espoo, Finland<p>The southern Finland granites and associated migmatitic rocks have a complex metamorphic history, being affected by multiple events during the ca. 1.88–1.79 Ga Svecofennian orogeny. In this study, the prolonged tectonic evolution of migmatites and associated rocks in southwestern Finland has been investigated using the new in situ Lu–Hf method. Results reveal detailed temporal constraints for the tectonic evolution that can be linked to major events in adjacent tectonic blocks in both Finland and Sweden during the Svecofennian orogeny. The metamorphic peak at the Olkiluoto site occurred at 1829 <span class="inline-formula">±</span> 19 Ma based on in situ Lu–Hf dating of garnet. The pressure–temperature (<span class="inline-formula"><i>P</i></span>–<span class="inline-formula"><i>T</i></span>) path for the rocks indicates a prograde evolution, with peak <span class="inline-formula"><i>P</i></span>–<span class="inline-formula"><i>T</i></span> conditions of 3–5 kbar and approximately 700 °C. Younger ages of ca. 1780 Ma obtained using both Lu–Hf and U–Pb systems in apatite inclusions in garnet indicate rapid cooling at 1780 Ma. Based on the metamorphic constraints and obtained ages, we link the Olkiluoto site to the Häme orogenic belt in southern Finland and also support the proposed thermal–tectonic connection with the Ljusdal lithotectonic unit in central Sweden.</p>https://se.copernicus.org/articles/16/97/2025/se-16-97-2025.pdf |
| spellingShingle | J. Engström J. Engström K. Cutts S. Glorie E. Heilimo E. M. Jolis R. M. Michallik Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland Solid Earth |
| title | Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland |
| title_full | Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland |
| title_fullStr | Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland |
| title_full_unstemmed | Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland |
| title_short | Insights into the tectonic evolution of the Svecofennian orogeny based on in situ Lu–Hf dating of garnet and apatite from Olkiluoto, southwestern Finland |
| title_sort | insights into the tectonic evolution of the svecofennian orogeny based on in situ lu hf dating of garnet and apatite from olkiluoto southwestern finland |
| url | https://se.copernicus.org/articles/16/97/2025/se-16-97-2025.pdf |
| work_keys_str_mv | AT jengstrom insightsintothetectonicevolutionofthesvecofennianorogenybasedoninsituluhfdatingofgarnetandapatitefromolkiluotosouthwesternfinland AT jengstrom insightsintothetectonicevolutionofthesvecofennianorogenybasedoninsituluhfdatingofgarnetandapatitefromolkiluotosouthwesternfinland AT kcutts insightsintothetectonicevolutionofthesvecofennianorogenybasedoninsituluhfdatingofgarnetandapatitefromolkiluotosouthwesternfinland AT sglorie insightsintothetectonicevolutionofthesvecofennianorogenybasedoninsituluhfdatingofgarnetandapatitefromolkiluotosouthwesternfinland AT eheilimo insightsintothetectonicevolutionofthesvecofennianorogenybasedoninsituluhfdatingofgarnetandapatitefromolkiluotosouthwesternfinland AT emjolis insightsintothetectonicevolutionofthesvecofennianorogenybasedoninsituluhfdatingofgarnetandapatitefromolkiluotosouthwesternfinland AT rmmichallik insightsintothetectonicevolutionofthesvecofennianorogenybasedoninsituluhfdatingofgarnetandapatitefromolkiluotosouthwesternfinland |