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230Th/U Chronology and Geochemistry of Irinovskoe Hydrothermal Field (Mid-Atlantic Ridge). / Kuznetsov, V. Yu; Tabuns, E. V.; Cherkashev, G. A.; Bel’tenev, V. E.; Maksimov, F. E.; Kuksa, K. A.; Lazareva, L. I.; Levchenko, S. B.; Zherebtsov, I. E.

In: Doklady Earth Sciences, Vol. 478, No. 1, 01.01.2018, p. 26-30.

Research output: Contribution to journal › Article › peer-review

Harvard

Kuznetsov, VY, Tabuns, EV, Cherkashev, GA, Bel’tenev, VE, Maksimov, FE, Kuksa, KA, Lazareva, LI, Levchenko, SB & Zherebtsov, IE 2018, '230Th/U Chronology and Geochemistry of Irinovskoe Hydrothermal Field (Mid-Atlantic Ridge)', Doklady Earth Sciences, vol. 478, no. 1, pp. 26-30. https://doi.org/10.1134/S1028334X18010142

APA

Kuznetsov, V. Y., Tabuns, E. V., Cherkashev, G. A., Bel’tenev, V. E., Maksimov, F. E., Kuksa, K. A., Lazareva, L. I., Levchenko, S. B., & Zherebtsov, I. E. (2018). 230Th/U Chronology and Geochemistry of Irinovskoe Hydrothermal Field (Mid-Atlantic Ridge). Doklady Earth Sciences, 478(1), 26-30. https://doi.org/10.1134/S1028334X18010142

Vancouver

Kuznetsov VY, Tabuns EV, Cherkashev GA, Bel’tenev VE, Maksimov FE, Kuksa KA et al. 230Th/U Chronology and Geochemistry of Irinovskoe Hydrothermal Field (Mid-Atlantic Ridge). Doklady Earth Sciences. 2018 Jan 1;478(1):26-30. https://doi.org/10.1134/S1028334X18010142

Author

Kuznetsov, V. Yu ; Tabuns, E. V. ; Cherkashev, G. A. ; Bel’tenev, V. E. ; Maksimov, F. E. ; Kuksa, K. A. ; Lazareva, L. I. ; Levchenko, S. B. ; Zherebtsov, I. E. / 230Th/U Chronology and Geochemistry of Irinovskoe Hydrothermal Field (Mid-Atlantic Ridge). In: Doklady Earth Sciences. 2018 ; Vol. 478, No. 1. pp. 26-30.

BibTeX

@article{359fb2cfc58a4c76a076ecddb1aaf961,
title = "230Th/U Chronology and Geochemistry of Irinovskoe Hydrothermal Field (Mid-Atlantic Ridge)",
abstract = "The results of 230Th/U dating and mineralogical–geochemical studies of sulfide ores from the Irinovskoe hydrothermal field and the Severo-Zapadnoe ore occurrence (Mid-Atlantic Ridge) are presented. Sulfides are represented primarily by copper–sulfide ores with 12–30% Cu content; sulfur- and zinc-sulfide ores are distributed less frequently. The analysis of a change in the composition of sulfides over time has made it possible to identify three stages of formation. Each stage assumes that mineral associations are changed from high-temperature (sulfur and copper sulfide) to medium temperature (Zn–Cu and Zn-sulfide) sulfide ores. The whole age range of formation of the hydrothermal deposits falls within the time interval of about 58000–8000 for the Irinovskoe field and 69000–11000 years ago for the Severo-Zapadnoe ore occurrence.",
author = "Kuznetsov, {V. Yu} and Tabuns, {E. V.} and Cherkashev, {G. A.} and Bel{\textquoteright}tenev, {V. E.} and Maksimov, {F. E.} and Kuksa, {K. A.} and Lazareva, {L. I.} and Levchenko, {S. B.} and Zherebtsov, {I. E.}",
year = "2018",
month = jan,
day = "1",
doi = "10.1134/S1028334X18010142",
language = "English",
volume = "478",
pages = "26--30",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - 230Th/U Chronology and Geochemistry of Irinovskoe Hydrothermal Field (Mid-Atlantic Ridge)

AU - Kuznetsov, V. Yu

AU - Tabuns, E. V.

AU - Cherkashev, G. A.

AU - Bel’tenev, V. E.

AU - Maksimov, F. E.

AU - Kuksa, K. A.

AU - Lazareva, L. I.

AU - Levchenko, S. B.

AU - Zherebtsov, I. E.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The results of 230Th/U dating and mineralogical–geochemical studies of sulfide ores from the Irinovskoe hydrothermal field and the Severo-Zapadnoe ore occurrence (Mid-Atlantic Ridge) are presented. Sulfides are represented primarily by copper–sulfide ores with 12–30% Cu content; sulfur- and zinc-sulfide ores are distributed less frequently. The analysis of a change in the composition of sulfides over time has made it possible to identify three stages of formation. Each stage assumes that mineral associations are changed from high-temperature (sulfur and copper sulfide) to medium temperature (Zn–Cu and Zn-sulfide) sulfide ores. The whole age range of formation of the hydrothermal deposits falls within the time interval of about 58000–8000 for the Irinovskoe field and 69000–11000 years ago for the Severo-Zapadnoe ore occurrence.

AB - The results of 230Th/U dating and mineralogical–geochemical studies of sulfide ores from the Irinovskoe hydrothermal field and the Severo-Zapadnoe ore occurrence (Mid-Atlantic Ridge) are presented. Sulfides are represented primarily by copper–sulfide ores with 12–30% Cu content; sulfur- and zinc-sulfide ores are distributed less frequently. The analysis of a change in the composition of sulfides over time has made it possible to identify three stages of formation. Each stage assumes that mineral associations are changed from high-temperature (sulfur and copper sulfide) to medium temperature (Zn–Cu and Zn-sulfide) sulfide ores. The whole age range of formation of the hydrothermal deposits falls within the time interval of about 58000–8000 for the Irinovskoe field and 69000–11000 years ago for the Severo-Zapadnoe ore occurrence.

UR - http://www.scopus.com/inward/record.url?scp=85042562225&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18010142

DO - 10.1134/S1028334X18010142

M3 - Article

AN - SCOPUS:85042562225

VL - 478

SP - 26

EP - 30

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 28671968