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Izotope (δ 13 C and δ 18 O) and genetic features of manganese carbonates of Mazul deposits (Krasnoyarsk region). / Kuleshov, V.N.; Zhukov, I.G.; Brusnitsyn, A.I.

In: Lithology and Mineral Resources, Vol. 52, No. 1, 2017, p. 51-60.

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Kuleshov, V.N. ; Zhukov, I.G. ; Brusnitsyn, A.I. / Izotope (δ 13 C and δ 18 O) and genetic features of manganese carbonates of Mazul deposits (Krasnoyarsk region). In: Lithology and Mineral Resources. 2017 ; Vol. 52, No. 1. pp. 51-60.

BibTeX

@article{601bee985333427e8026145782c4e82e,
title = "Izotope (δ 13 C and δ 18 O) and genetic features of manganese carbonates of Mazul deposits (Krasnoyarsk region)",
abstract = "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.",
author = "V.N. Kuleshov and I.G. Zhukov and A.I. Brusnitsyn",
year = "2017",
doi = "10.1134/S0024490217010047",
language = "English",
volume = "52",
pages = "51--60",
journal = "Lithology and Mineral Resources",
issn = "0024-4902",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - Izotope (δ 13 C and δ 18 O) and genetic features of manganese carbonates of Mazul deposits (Krasnoyarsk region)

AU - Kuleshov, V.N.

AU - Zhukov, I.G.

AU - Brusnitsyn, A.I.

PY - 2017

Y1 - 2017

N2 - 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.

AB - 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.

U2 - 10.1134/S0024490217010047

DO - 10.1134/S0024490217010047

M3 - Article

VL - 52

SP - 51

EP - 60

JO - Lithology and Mineral Resources

JF - Lithology and Mineral Resources

SN - 0024-4902

IS - 1

ER -

ID: 7757005