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230Th/U chronology of ore formation within the Semyenov hydrothermal district (13 o 31’ N) at the Mid-Atlantic Ridge. / Kuznetsov, V.; Maksimov, F.; Zheleznov, A.; Cherkashov, G.; Bel’tenev, V.; Lazareva, L.

в: Geochronometria, Том 38, № 1, 2011, стр. 72-76.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Kuznetsov, V, Maksimov, F, Zheleznov, A, Cherkashov, G, Bel’tenev, V & Lazareva, L 2011, '230Th/U chronology of ore formation within the Semyenov hydrothermal district (13 o 31’ N) at the Mid-Atlantic Ridge', Geochronometria, Том. 38, № 1, стр. 72-76. https://doi.org/10.2478/s13386-011-0001-1

APA

Kuznetsov, V., Maksimov, F., Zheleznov, A., Cherkashov, G., Bel’tenev, V., & Lazareva, L. (2011). 230Th/U chronology of ore formation within the Semyenov hydrothermal district (13 o 31’ N) at the Mid-Atlantic Ridge. Geochronometria, 38(1), 72-76. https://doi.org/10.2478/s13386-011-0001-1

Vancouver

Kuznetsov V, Maksimov F, Zheleznov A, Cherkashov G, Bel’tenev V, Lazareva L. 230Th/U chronology of ore formation within the Semyenov hydrothermal district (13 o 31’ N) at the Mid-Atlantic Ridge. Geochronometria. 2011;38(1):72-76. https://doi.org/10.2478/s13386-011-0001-1

Author

Kuznetsov, V. ; Maksimov, F. ; Zheleznov, A. ; Cherkashov, G. ; Bel’tenev, V. ; Lazareva, L. / 230Th/U chronology of ore formation within the Semyenov hydrothermal district (13 o 31’ N) at the Mid-Atlantic Ridge. в: Geochronometria. 2011 ; Том 38, № 1. стр. 72-76.

BibTeX

@article{87c13785224e4c909dc4ba5e438c8105,
title = "230Th/U chronology of ore formation within the Semyenov hydrothermal district (13 o 31{\textquoteright} N) at the Mid-Atlantic Ridge",
abstract = "A radiochemical study was carried out on massive sulfides from Semyenov hydrothermal district at the Mid-Atlantic Ridge. New and published results provide evidence that 230Th/U ages ob-tained for massive sulfides are reliable. The sulfide deposits from the West, North-West, North-East, and East hydrothermal sites at the Semyenov hydrothermal district were formed between ~124 ka and ~37 ka ago. The hydrothermal activity might have started in the eastern part of the district and moved to the west by episodic ore formation.",
keywords = "geochronology, Mid-Atlantic Ridge, hydrothermal vents, massive sulfides",
author = "V. Kuznetsov and F. Maksimov and A. Zheleznov and G. Cherkashov and V. Bel{\textquoteright}tenev and L. Lazareva",
year = "2011",
doi = "10.2478/s13386-011-0001-1",
language = "English",
volume = "38",
pages = "72--76",
journal = "Geochronometria",
issn = "1733-8387",
publisher = "De Gruyter",
number = "1",

}

RIS

TY - JOUR

T1 - 230Th/U chronology of ore formation within the Semyenov hydrothermal district (13 o 31’ N) at the Mid-Atlantic Ridge

AU - Kuznetsov, V.

AU - Maksimov, F.

AU - Zheleznov, A.

AU - Cherkashov, G.

AU - Bel’tenev, V.

AU - Lazareva, L.

PY - 2011

Y1 - 2011

N2 - A radiochemical study was carried out on massive sulfides from Semyenov hydrothermal district at the Mid-Atlantic Ridge. New and published results provide evidence that 230Th/U ages ob-tained for massive sulfides are reliable. The sulfide deposits from the West, North-West, North-East, and East hydrothermal sites at the Semyenov hydrothermal district were formed between ~124 ka and ~37 ka ago. The hydrothermal activity might have started in the eastern part of the district and moved to the west by episodic ore formation.

AB - A radiochemical study was carried out on massive sulfides from Semyenov hydrothermal district at the Mid-Atlantic Ridge. New and published results provide evidence that 230Th/U ages ob-tained for massive sulfides are reliable. The sulfide deposits from the West, North-West, North-East, and East hydrothermal sites at the Semyenov hydrothermal district were formed between ~124 ka and ~37 ka ago. The hydrothermal activity might have started in the eastern part of the district and moved to the west by episodic ore formation.

KW - geochronology

KW - Mid-Atlantic Ridge

KW - hydrothermal vents

KW - massive sulfides

U2 - 10.2478/s13386-011-0001-1

DO - 10.2478/s13386-011-0001-1

M3 - Article

VL - 38

SP - 72

EP - 76

JO - Geochronometria

JF - Geochronometria

SN - 1733-8387

IS - 1

ER -

ID: 5056288