Geochronological evidence for late‐Grenvillian magmatic and metamorphic events in central Taimyr, northern Siberia *

• Published in: Terra Nova
• Main Authors: Pease, V., Gee, D. G., Vernikovsky, V., Vernikovskaya, A., Kireev, S.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2001
• Subjects: Arctic; Greenland; Shrenk; East Greenland; Taimyr; Siberia
• Online Access: http://dx.doi.org/10.1046/j.1365-3121.2001.00351.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.2001.00351.x; https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.2001.00351.x

U–Th–Pb analyses of zircons from six granites and one metasediment collected in the accretionary Central belt of Taimyr, Arctic Siberia, demonstrate that Neoproterozoic ( c . 900 Ma) granites intrude late Mesoproterozoic/early Neoproterozoic amphibolite facies metamorphic rocks. This is the first time in the Mamont–Shrenk region that Neoproterozoic ages have been recognized for these lithologies, previously thought to be Archaean/Palaeoproterozoic in age. The Mamont–Shrenk Terrane (MST) represents a Grenvillian age (micro?) continent intercalated with younger Neoproterozoic ophiolites during thrusting and accreted to the northern margin of the Siberian craton sometime before the late Vendian. Basement to the MST may have been derived from the Grenvillian belt of east Greenland. Viable tectonic reconstructions must allow for an active margin along northern Siberia (modern day coordinates) in the middle Neoproterozoic.