Common Neoproterozoic–Early Paleozoic Evolution of Ore-Bearing Sedimentary Complexes in the Southern Siberian Craton


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Abstract

A comparison of the lithological–geochemical parameters for the deposits of the Dalnetaiga series of the Bodaibo synclinorium (the Buzhuikhta and Khomolkho formations) and the Olokit structural-formational zone (the Itykit and Ondok formations), hosting polymetallic deposits (Kholodnin, Ioko-Rybach’e), along with the obtained geochronological LA-ICP-MS U–Pb age estimates of the Ondok Formation (~600 Ma), indicates their similar stratigraphic position in the Neoproterozoic in Southern Siberia. At the first stage of formation of polymetallic and gold-ore objects, the siderochalcophylic trend is considered to have appeared synchronously in the two structural zones, which could have been caused by the hydrothermal activity in the back-arc basin of the Olokit structure.

About the authors

A. E. Budyak

Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences; Irkutsk Science Center, Siberian Branch, Russian Academy of Sciences

Author for correspondence.
Email: budyak@igc.irk.ru
Russian Federation, Irkutsk, 664033; Irkutsk, 664033

S. Yu. Skuzovatov

Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences; Institute of Earth Sciences, Academia Sinica

Email: budyak@igc.irk.ru
Russian Federation, Irkutsk, 664033; Taipei

Yu. I. Tarasova

Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences; Irkutsk National Research Technical University

Email: budyak@igc.irk.ru
Russian Federation, Irkutsk, 664033; Irkutsk, 664074

Kuo-Lung Wang

Institute of Earth Sciences, Academia Sinica

Email: budyak@igc.irk.ru
Taiwan, Province of China, Taipei

N. A. Goryachev

Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences; Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch, Russian Academy of Sciences

Email: budyak@igc.irk.ru
Russian Federation, Irkutsk, 664033; Magadan, 685000


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