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Chronology of seafloor massive sulfides formation within the Pobeda hydrothermal cluster (Mid-Atlantic Ridge). / Kuznetsov , V. ; Cherkashov, G.; Kuksa, K. ; Firstova, A. ; Maksimov, F. ; Bel’Tenev, V. ; Lazareva, L. ; Levchenko , S. ; Baranova, N. .

In: Geochronometria, Vol. 47, No. 1, 12.2020, p. 63-70.

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

Harvard

Kuznetsov , V, Cherkashov, G, Kuksa, K, Firstova, A, Maksimov, F, Bel’Tenev, V, Lazareva, L, Levchenko , S & Baranova, N 2020, 'Chronology of seafloor massive sulfides formation within the Pobeda hydrothermal cluster (Mid-Atlantic Ridge)', Geochronometria, vol. 47, no. 1, pp. 63-70. https://doi.org/10.2478/geochr-2020-0019

APA

Kuznetsov , V., Cherkashov, G., Kuksa, K., Firstova, A., Maksimov, F., Bel’Tenev, V., Lazareva, L., Levchenko , S., & Baranova, N. (2020). Chronology of seafloor massive sulfides formation within the Pobeda hydrothermal cluster (Mid-Atlantic Ridge). Geochronometria, 47(1), 63-70. https://doi.org/10.2478/geochr-2020-0019

Vancouver

Kuznetsov V, Cherkashov G, Kuksa K, Firstova A, Maksimov F, Bel’Tenev V et al. Chronology of seafloor massive sulfides formation within the Pobeda hydrothermal cluster (Mid-Atlantic Ridge). Geochronometria. 2020 Dec;47(1):63-70. https://doi.org/10.2478/geochr-2020-0019

Author

Kuznetsov , V. ; Cherkashov, G. ; Kuksa, K. ; Firstova, A. ; Maksimov, F. ; Bel’Tenev, V. ; Lazareva, L. ; Levchenko , S. ; Baranova, N. . / Chronology of seafloor massive sulfides formation within the Pobeda hydrothermal cluster (Mid-Atlantic Ridge). In: Geochronometria. 2020 ; Vol. 47, No. 1. pp. 63-70.

BibTeX

@article{ff351ac7483f41e29af31a7f99085f88,
title = "Chronology of seafloor massive sulfides formation within the Pobeda hydrothermal cluster (Mid-Atlantic Ridge)",
abstract = "A geochronological and mineralogical study on the seafloor massive sulfides from the Pobeda hydrothermal cluster at the Mid-Atlantic Ridge was carried out. To improve the reliability of geochronological data, the 230Th/U ages were measured for both the bulk samples and monomineral separates. The oldest age ca. 52 kyr within Pobeda-1 and ca. 107 kyr within Pobeda–2 fields have been obtained. Then, several episodes of hydrothermal activity were identified within both fields up to ca. 0.3 kyr ago and up to ca. 4.3 kyr ago, respectively. ",
keywords = "geochronology, hydrothermal activity, 230Th/U dating, seafloor massive sulfides.",
author = "V. Kuznetsov and G. Cherkashov and K. Kuksa and A. Firstova and F. Maksimov and V. Bel{\textquoteright}Tenev and L. Lazareva and S. Levchenko and N. Baranova",
year = "2020",
month = dec,
doi = "10.2478/geochr-2020-0019",
language = "English",
volume = "47",
pages = "63--70",
journal = "Geochronometria",
issn = "1733-8387",
publisher = "De Gruyter",
number = "1",

}

RIS

TY - JOUR

T1 - Chronology of seafloor massive sulfides formation within the Pobeda hydrothermal cluster (Mid-Atlantic Ridge)

AU - Kuznetsov , V.

AU - Cherkashov, G.

AU - Kuksa, K.

AU - Firstova, A.

AU - Maksimov, F.

AU - Bel’Tenev, V.

AU - Lazareva, L.

AU - Levchenko , S.

AU - Baranova, N.

PY - 2020/12

Y1 - 2020/12

N2 - A geochronological and mineralogical study on the seafloor massive sulfides from the Pobeda hydrothermal cluster at the Mid-Atlantic Ridge was carried out. To improve the reliability of geochronological data, the 230Th/U ages were measured for both the bulk samples and monomineral separates. The oldest age ca. 52 kyr within Pobeda-1 and ca. 107 kyr within Pobeda–2 fields have been obtained. Then, several episodes of hydrothermal activity were identified within both fields up to ca. 0.3 kyr ago and up to ca. 4.3 kyr ago, respectively.

AB - A geochronological and mineralogical study on the seafloor massive sulfides from the Pobeda hydrothermal cluster at the Mid-Atlantic Ridge was carried out. To improve the reliability of geochronological data, the 230Th/U ages were measured for both the bulk samples and monomineral separates. The oldest age ca. 52 kyr within Pobeda-1 and ca. 107 kyr within Pobeda–2 fields have been obtained. Then, several episodes of hydrothermal activity were identified within both fields up to ca. 0.3 kyr ago and up to ca. 4.3 kyr ago, respectively.

KW - geochronology, hydrothermal activity, 230Th/U dating, seafloor massive sulfides.

U2 - 10.2478/geochr-2020-0019

DO - 10.2478/geochr-2020-0019

M3 - Article

VL - 47

SP - 63

EP - 70

JO - Geochronometria

JF - Geochronometria

SN - 1733-8387

IS - 1

ER -

ID: 72539072