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

V. Yu Kuznetsov, E. V. Tabuns, G. A. Cherkashev, V. E. Bel’tenev, F. E. Maksimov, K. A. Kuksa, L. I. Lazareva, S. B. Levchenko, I. E. Zherebtsov

Результат исследований: Научные публикации в периодических изданияхстатья

Выдержка

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.

Язык оригиналаанглийский
Страницы (с-по)26-30
Число страниц5
ЖурналDoklady Earth Sciences
Том478
Номер выпуска1
DOI
СостояниеОпубликовано - 1 янв 2018

Отпечаток

chronology
geochemistry
sulfide
sulfur
hydrothermal deposit
ore
zinc
copper
mineral
temperature

Предметные области Scopus

  • Планетоведение и науки о земле (разное)
  • Планетоведение и науки о земле (все)

Цитировать

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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.",
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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.

В: Doklady Earth Sciences, Том 478, № 1, 01.01.2018, стр. 26-30.

Результат исследований: Научные публикации в периодических изданияхстатья

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

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