Long-lived connection between southern Siberia and northern Laurentia in the Proterozoic
Autor: | A. V. Okrugin, Kenneth L. Buchan, Wouter Bleeker, J. A. Hanes, Kevin R. Chamberlain, Dmitry P. Gladkochub, Ulf Söderlund, A. N. Didenko, Richard E. Ernst, A. S. Mekhonoshin, A N LeCheminant, Michael A. Hamilton, T. B. Kolotilina |
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Rok vydání: | 2016 |
Předmět: |
geography
Paleomagnetism geography.geographical_feature_category 010504 meteorology & atmospheric sciences Proterozoic Earth science Large igneous province протерозой 010502 geochemistry & geophysics 01 natural sciences суперконтиненты Paleontology Precambrian Igneous rock Лаврентия континет Sill Rodinia Южная Сибирь General Earth and Planetary Sciences Laurentia тектоника плит Geology 0105 earth and related environmental sciences |
Zdroj: | Nature geoscience. 2016. Vol. 9, № 6. P. 464-469 |
ISSN: | 1752-0908 1752-0894 |
DOI: | 10.1038/ngeo2700 |
Popis: | Precambrian supercontinents Nuna-Columbia (1.7 to 1.3 billion years ago) and Rodinia (1.1 to 0.7 billion years ago) have been proposed. However, the arrangements of crustal blocks within these supercontinents are poorly known. Huge, dominantly basaltic magmatic outpourings and intrusions, covering up to millions of square kilometres, termed Large Igneous Provinces, typically accompany (super) continent breakup, or attempted breakup and offer an important tool for reconstructing supercontinents. Here we focus on the Large Igneous Province record for Siberia and Laurentia, whose relative position in Nuna-Columbia and Rodinia reconstructions is highly controversial. We present precise geochronology—nine U–Pb and six Ar–Ar ages—on dolerite dykes and sills, along with existing dates from the literature, that constrain the timing of emplacement of Large Igneous Province magmatism in southern Siberia and northern Laurentia between 1,900 and 720 million years ago. We identify four robust age matches between the continents 1,870, 1,750, 1,350 and 720 million years ago, as well as several additional approximate age correlations that indicate southern Siberia and northern Laurentia were probably near neighbours for this 1.2-billion-year interval. Our reconstructions provide a framework for evaluating the shared geological, tectonic and metallogenic histories of these continental blocks. The configurations of the ancient supercontinents are poorly known. Analysis of the ages of giant magma intrusions that affected both Siberia and Laurentia shows that the two continents were connected, possibly for as long as 1.2 billion years. |
Databáze: | OpenAIRE |
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