Australia: The Land Where Time Began |
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Siberia and Laurentia – Long-Lived Connection between Southern
Siberia and Northern Laurentia in the Proterozoic
Nuna-Columbia (1.7-1.3 Ga) and Rodinia 1.1- 0.7 Ga) are supercontinents
that have been proposed to have existed in the Precambrian. It is poorly
known how the crustal blocks were arranged within these supercontinents.
An important tool for the reconstruction of supercontinents are the
magmatic outpourings and intrusions, that are dominantly basaltic, that
cover areas of up to millions of square kilometres, that are termed
Large Igneous Provinces, which typically accompany the breakup, or
abortive breakup, of (super) continents. In this paper Ernst et
al. present the results of
their study that focused on the Large Igneous Province record from
Siberia and Laurentia, the reconstructions of the relative positions of
these landmasses in Nuna-Columbia and Rodinia which is highly
controversial. Precise geochronology (9 U-Pb and 6 Ar-Ar ages) on
dolerite dykes and sills, as well as existing dates from the literature,
that constrain the emplacement of Large Igneous Province magmatism in
southern Siberia and northern Laurentia between 1.9 Ga and 700 Ma. There
are 4 robust age matches between the continents 1.87, 1.75, 1.35 Ga and
700 Ma, as well as several additional age correlations which are
approximate, indicating that it is probable that southern Siberia and
northern Laurentia were near neighbours for this interval of 1.2 Gyr. A
framework for evaluating the shared geological, tectonic and
metallogenic histories of these continental blocks has been provided by
these reconstructions.
Ernst, R. E., M. A. Hamilton, U. Soderlund, J. A. Hanes, D. P.
Gladkochub, A. V. Okrugin, T. Kolotilina, A. S. Mekhonoshin, W. Bleeker,
A. N. LeCheminant, K. L. Buchan, K. R. Chamberlain and A. N. Didenko
(2016). "Long-lived
connection between southern Siberia and northern Laurentia in the
Proterozoic." Nature Geosci 9(6): 464-469.
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Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading |