Is there a 1.85Ga magmatic event in northern Norrbotten? - U-Pb SIMS zircon dating of the Pingisvaara metagranodiorite and the Jyryjoki granite, northern Sweden

被引:4
|
作者
Hellstrom, Fredrik A. [1 ]
Bergman, Stefan [1 ]
机构
[1] Geol Survey Sweden, Dept Mineral Resources, Uppsala, Sweden
关键词
U-Pb; SIMS; zircon; geochronology; Pingisvaara metagranodiorite; Jyryjoki granite; igneous crystallisation; metamorphism; Svecokarelian orogen; CENTRAL FENNOSCANDIAN SHIELD; PAJALA SHEAR ZONE; ION-MICROPROBE; TRACE-ELEMENT; TH-PB; AGE; GEOCHRONOLOGY; REACTIVATION; DEFORMATION; CONSTRAINTS;
D O I
10.1080/11035897.2016.1171254
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Previously published discordant U-Pb zircon TIMS data of two granitoids from northern Sweden are here reassessed based on new U-Pb data acquired using the SIMS method. Zircon from the Pingisvaara metagranodiorite consists of older domains representing igneous crystallisation at 1881 +/- 5Ma and younger metamorphic domains dated at 1827 +/- 4Ma. The previous TIMS-age of 1856 +/- 8Ma for this sample is rejected. The previous, poorly constrained age determination of the Jyryjoki granite at 1853 +/- 21Ma, obtained by TIMS-analyses is herein improved using SIMS-technique. The new age at 1853 +/- 4Ma is interpreted to date igneous crystallisation of the granite. While 1.86-1.85Ga intrusive rocks are rare in northernmost Sweden there is growing evidence for metamorphic and hydrothermal activity in that time interval. The metamorphism at 1.83-1.82Ga recorded in zircon from the Pingisvaara metagranodiorite is consistent with a previously suggested protracted metamorphic event between 1.83 and 1.77Ga.
引用
收藏
页码:526 / 532
页数:7
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