Isotope (δ13C and δ18O) and genetic features of manganese carbonates of the Mazul deposit (Krasnoyarsk region)


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New isotope and mineral data on manganese carbonates of the Mazul deposit (Krasnoyarsk region) in combination with morphology of ore bodies suggest that the ores were formed in several stages with the involvement of meteoric solutions through infiltration and, possibly, exfiltration mechanisms. Based on the geological–geochemical data, manganese carbonates of the Mazul deposit may be ascribed to a new genetic subtype of the catagenesis (epigenesis) zone.

作者简介

V. Kuleshov

Geological Institute

编辑信件的主要联系方式.
Email: vnkuleshov@mail.ru
俄罗斯联邦, Pyzhevskii per. 7, Moscow, 119017

I. Zhukov

Institute of Mineralogy, Ural Branch; National Research Branch

Email: vnkuleshov@mail.ru
俄罗斯联邦, Miass, Chelyabinsk oblast, 456317; Miass, Chelyabisnk oblast, 456318

A. Brusnitsyn

Faculty of Geology

Email: vnkuleshov@mail.ru
俄罗斯联邦, Universitetskaya nab. 7/9, St. Petersburg, 199034

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