Doklady Earth Sciences

, Volume 476, Issue 1, pp 1010–1015 | Cite as

New hydrothermal sulfide fields of the Mid-Atlantic Ridge: Yubileinoe (20°09′ N) and Surprise (20°45.4′ N)

  • V. E. Bel’tenev
  • L. I. Lazareva
  • G. A. Cherkashev
  • V. I. Ivanov
  • I. I. Rozhdestvenskaya
  • V. A. Kuznetsov
  • A. A. Laiba
  • E. V. Narkevskiy
Geology
  • 38 Downloads

Abstract

Two new sulfide fields (Yubileinoe, 20°09′ N, and Surprise, 20°45.4′ N) were discovered between 20°01′ and 20°54′ N within the Russian Application Area of the Mid-Atlantic Ridge (MAR). The Yubileinoe field is located at a depth of 2300–2550 m in the near-top area of the first rift ridge, which is a boundary of the western wall of the rift valley. This new field and the Zenith-Victory field, which was previously discovered in the eastern wall, occur symmetrically relative to the rift valley of this MAR segment. The Surprise field at a depth of 2800–2850 m is situated in the eastern wall of the rift valley, on the slope of the volcanic uplift. After the discovery of these inactive sulfide fields, the number of hydrothermal fields within the Russian Application Area reached ten.

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Copyright information

© Pleiades Publishing, Ltd. 2017

Authors and Affiliations

  • V. E. Bel’tenev
    • 1
  • L. I. Lazareva
    • 1
  • G. A. Cherkashev
    • 2
    • 3
  • V. I. Ivanov
    • 1
  • I. I. Rozhdestvenskaya
    • 1
  • V. A. Kuznetsov
    • 3
  • A. A. Laiba
    • 1
  • E. V. Narkevskiy
    • 1
  1. 1.Polar Marine Geosurvey ExpeditionLomonosov–St. PetersburgRussia
  2. 2.Gramberg All-Russia Research Institute of Geology and Mineral Resources of the World OceanSt. PetersburgRussia
  3. 3.Institute of Earth SciencesSt. Petersburg State UniversitySt. PetersburgRussia

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