A Search for Sources of the Detritus of Ordovician Sandstones from the Sol-Iletsk Block (Ordovician-2 Borehole) Based on the First Data of the Geochemical and Lu/Hf Isotopic Systematics of Zircons


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Abstract

The primary isotope–geochemical and geochemical characteristics (by the TerraneChrone® technique) are presented for detrital zircons dated previously (U/Pb, LA–ICP–MS dating) from Ordovician sandstones (the Ordovician-2 borehole of the Sol-Iletsk block). The characteristics of the treated zircons were compared to the corresponding parameters of the complexes constituting the possible sources provinces.

About the authors

T. V. Romanyuk

Schmidt Institute of Physics of the Earth, Russian Academy
of Sciences; Australian Research Council Center of Excellence for Core
to Crust Fluid systems/GEMOS, Macquarie University; Gubkin Russian State University of Oil and Gas

Author for correspondence.
Email: t.romanyuk@mail.ru
Russian Federation, Moscow, 123995; Sydney; Moscow, 119991

E. A. Belousova

Australian Research Council Center of Excellence for Core
to Crust Fluid systems/GEMOS, Macquarie University

Email: t.romanyuk@mail.ru
Australia, Sydney

N. B. Kuznetsov

Australian Research Council Center of Excellence for Core
to Crust Fluid systems/GEMOS, Macquarie University; Gubkin Russian State University of Oil and Gas; Geological Institute, Russian Academy of Sciences

Email: t.romanyuk@mail.ru
Australia, Sydney; Moscow, 119991; Moscow, 119017

V. M. Gorozhanin

Institute of Geology, Ural Branch, Russian Academy
of Sciences; Bashkir State University

Email: t.romanyuk@mail.ru
Russian Federation, Ufa, 450077; Ufa

E. N. Gorozhanina

Institute of Geology, Ural Branch, Russian Academy
of Sciences

Email: t.romanyuk@mail.ru
Russian Federation, Ufa, 450077

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