Sveconorwegian crustal underplating in southwestern Fennoscandia:LAM-ICPMS U-Pb and Lu-Hf isotope evidence from granites and gneisses in Telemark, southern Norway

• Published in: Lithos
• Main Authors: Andersen, T., Griffin, W. L., Sylvester, A. G.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2007
• Subjects: Fennoscandian
• Online Access: https://researchers.mq.edu.au/en/publications/cd32e8df-05f5-45ed-b7ce-938641f847a0; https://doi.org/10.1016/j.lithos.2006.03.068; http://www.scopus.com/inward/record.url?scp=33846175690&partnerID=8YFLogxK

Laser ablation ICPMS U-Pb and Lu-Hf isotope data on granitic-granodioritic gneisses of the Precambrian Vråvatn complex in central Telemark, southern Norway, indicate that the magmatic protoliths crystallized at 1201 ± 9 Ma to 1219 ± 8 Ma, from magmas with juvenile or near-juvenile Hf isotopic composition ( 176 Hf/ 177 Hf = 0.2823 ± 11, epsilon-Hf > + 6). These data provide supporting evidence for the depleted mantle Hf-isotope evolution curve in a time period where juvenile igneous rocks are scarce on a global scale. They also identify a hitherto unknown event of mafic underplating in the region, and provide new and important limits on the crustal evolution of the SW part of the Fennoscandian Shield. This juvenile geochemical component in the deep crust may have contributed to the 1.0-0.92 Ga anorogenic magmatism in the region, which includes both A-type granite and a large anorthosite-mangerite-charnockite-granite intrusive complex. The gneisses of the Vråvatn complex were intruded by a granitic pluton with mafic enclaves and hybrid facies (the Vrådal granite) in that period. LAM-ICPMS U-Pb data from zircons from granitic and hybrid facies of the pluton indicates an intrusive age of 966 ± 4 Ma, and give a hint of ca. 1.46 Ga inheritance. The initial Hf isotopic composition of this granite ( 176 Hf/ 177 Hf = 0.28219 ± 13, epsilon-Hf = - 5 to + 6) overlaps with mixtures of pre-1.7 Ga crustal rocks and juvenile Sveconorwegian crust, lithospheric mantle and/or global depleted mantle. Contributions from ca. 1.2 Ga crustal underplate must be considered when modelling the petrogenesis of late Sveconorwegian anorogenic magmatism in the region.