Late Neoproterozoic granulite facies metamorphism of the Upper Gneiss unit (Seve Nappe Complex) in the V&#225;ivan&#269;ohkka-Salmme&#269;ohkat area, northern Scandinavian Caledonides&#160;
Authors: Callegari Riccardo , Walczak Katarzyna , Ziemniak Grzegorz , Barnes Christopher , Majka Jaroslaw 
Published: March 2021

&lt;p&gt;Here, we present preliminary petrochronological results of paragneisses and schists containing bodies of metamafic rocks belonging the Upper Gneiss unit that occurs within the Seve Nappe Complex (SNC) in the V&amp;#225;ivan&amp;#269;ohkka-Salmme&amp;#269;ohkat area, north of the lake Tornetr&amp;#228;sk in northern Sweden and Norway.&lt;/p&gt;&lt;p&gt;At the outcrop scale, the paragneiss is pervasively foliated and bears features of migmatization. It hosts garnet amphibolite bodies that are locally transected by leucocratic veins. Thin section observations of the paragneiss reveal a mineral assemblage composed of Q+Grt+Amp+Bi&amp;#177;Pl&amp;#177;Ms&amp;#177;Sil&amp;#177;Ru. The leucocratic vein contains Q+Pl+Ms+Bi+Grt+Kfs&amp;#177;Sil. Importantly, some of the studied gneisses contain quartz, exhibiting lobate boundaries, as well as garnet surrounded by melt rim. The presence of quartz forming pseudomorphs after melt was also identified and observed to host both monophase and fluid inclusions. All of these microtextures are indicative of partial melting.&lt;/p&gt;&lt;p&gt;Preliminary pressure-temperature estimates derived using conventional geothermobarometry and phase equilibrium modelling corroborated petrographic observations. The peak metamorphic conditions were estimated to 8&amp;#8211;10kbar and 800&amp;#8211;850&amp;#176;C, i.e., in the stability field of melt.&lt;/p&gt;&lt;p&gt;Uranium-Pb zircon and Th-U-total Pb monazite dating of the migmatitic paragneiss yielded consistent age estimates of 602&amp;#177;5Ma and 599&amp;#177;3Ma, respectively. Nearly the same U-Pb age of 604&amp;#177;7Ma was obtained for the zircon from the leucocratic vein transecting the amphibolite within the studied gneiss. Interestingly, no Caledonian zircon nor monazite were identified. Considering the textural position of the dated zircon and monazite, as well as their chemical character, we suggest that these minerals date the partial melting event recorded by the rocks.&lt;/p&gt;&lt;p&gt;Regionally, we interpret that the Upper Gneiss unit of SNC in the V&amp;#225;ivan&amp;#269;ohkka-Salmme&amp;#269;ohkat area could be a northern continuation of the Leavasv&amp;#225;ggi gneiss associated with the Vassa&amp;#269;oru Igneous Complex of SNC in the Kebnekaise region. Notably, the latter reveals evidence of high temperature metamorphism at c. 600Ma (Paulsson and Andr&amp;#233;asson 2002) and its mafic component (see also Rousku et al. in this session) could be an equivalent to the metamafic rocks enclosed within the Upper Gneiss unit. The Leavasv&amp;#225;ggi gneiss and the Upper Gneiss unit together with similar rocks farther north in Indre Troms and in Corrovare which also yield a c. 610-600Ma age of high grade overprint (Gee et al. 2016; Kj&amp;#248;ll et al. 2019). Altogether, these areas with only localized Caledonian influence diverge from traditional models developed for the SNC farther south and offer an additional insight into the development of the late Neoproterozoic margin of Baltica at the early stages of Iapetus opening.&lt;/p&gt;&lt;p&gt;This study was supported by the National Science Centre (Poland) grant no. 2019/33/B/ST10/01728 to J. Majka.&lt;/p&gt;&lt;p&gt;References&lt;/p&gt;&lt;p&gt;Gee et al. 2016. Baltoscandian margin, Sveconorwegian crust lost by subduction during Caledonian collisional orogeny. GFF 139, 36&amp;#8211;51.&lt;/p&gt;&lt;p&gt;Kj&amp;#248;ll et al. 2019. Timing of break-up and thermal evolution of a pre-Caledonian&amp;#160; Neoproterozoic exhumed magma-rich rifted margin. Tectonics 38, 1843-1862.&lt;/p&gt;&lt;p&gt;Paulsson &amp; Andr&amp;#233;asson 2002. Attempted break-up of Rodinia at 850 Ma: geochronological evidence from the Seve&amp;#8211;Kalak Superterrane, Scandinavian Caledonides. JGS, 159, 751-761.&lt;/p&gt;