Source Provenance and Paleogeographic Conditions during Deposition of Jurassic Continental Sediments in the Southern Part of the Siberian Platform (Implication ... View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2018-06

AUTHORS

E. I. Demonterova, A. V. Ivanov, E. A. Mikheeva, A. V. Arzhannikova, A. O. Frolov, S. G. Arzhannikov, N. V. Bryanskiy, L. A. Pavlova, L. Z. Reznitskii, O. V. Zarubina

ABSTRACT

The first Sm–Nd isotopic data and U–Pb (LA–ICP–MS) detrital zircon ages from sandstones of the Prisayan and Kuda Formations (the Irkutsk Basin, southern part of the Siberian Platform) have been obtained. They demonstrate that during accumulation of the sediments in the Irkutsk Basin, the contribution of local erosion sources decreased over time, while input from the Paleo–Transbaikalia sources increased. The change in provenance areas was triggered by tectonic rebuilding in Paleo–Transbaikalia caused by the closure of the Mongol–Okhotsk Ocean. More... »

PAGES

720-724

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1028334x18060235

DOI

http://dx.doi.org/10.1134/s1028334x18060235

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1105597212


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