![PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi](https://www.researchgate.net/profile/Raimo-Lahtinen/publication/292593395/figure/fig1/AS:990285056200718@1613113764530/Simplified-geological-map-ofthe-Rautalampi-area-based-on-the-map-by-Paeaejaervi-199-1-and_Q320.jpg)
PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi
![PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi](https://i1.rgstatic.net/publication/292593395_Crustal_evolution_of_the_Svecofennian_and_Karelian_domains_during_21-179_Ga_with_special_emphasis_on_the_geochemistry_and_origin_of_193-191_Ga_gneissic_tonalites_and_associated_supracrustal_rocks_in_t/links/60262940a6fdcc37a81d6e83/largepreview.png)
PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi
![PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi](https://www.researchgate.net/profile/Raimo-Lahtinen/publication/292593395/figure/tbl1/AS:990285060374529@1613113765342/Selected-major-anhydrous-and-trace-element-data-for-gneissic-tonalites-and-felsic_Q320.jpg)
PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi
![PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi PDF) Crustal evolution of the Svecofennian and Karelian domains during 2.1-1.79 Ga, with special emphasis on the geochemistry and origin of 1.93-1.91 Ga gneissic tonalites and associated supracrustal rocks in the Rautalampi](https://www.researchgate.net/profile/Raimo-Lahtinen/publication/292593395/figure/fig2/AS:990285056204803@1613113764572/Total-alkali-sili-ca-TAS-diagram-Le-Bas-el-al-1986-for-mafic-volcanics-inclusions_Q320.jpg)