Research output: Contribution to journal › Article › peer-review
New hydrothermal sulfide fields of the Mid-Atlantic Ridge : Yubileinoe (20°09′ N) and Surprise (20°45.4′ N). / Bel’tenev, V. E.; Lazareva, L. I.; Cherkashev, G. A.; Ivanov, V. I.; Rozhdestvenskaya, I. I.; Kuznetsov, V. Y.; Laiba, A. A.; Narkevskiy, E. V.
In: Doklady Earth Sciences, Vol. 476, No. 1, 01.09.2017, p. 1010-1015.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - New hydrothermal sulfide fields of the Mid-Atlantic Ridge
T2 - Yubileinoe (20°09′ N) and Surprise (20°45.4′ N)
AU - Bel’tenev, V. E.
AU - Lazareva, L. I.
AU - Cherkashev, G. A.
AU - Ivanov, V. I.
AU - Rozhdestvenskaya, I. I.
AU - Kuznetsov, V. Y.
AU - Laiba, A. A.
AU - Narkevskiy, E. V.
PY - 2017/9/1
Y1 - 2017/9/1
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=85030719874&partnerID=8YFLogxK
U2 - 10.1134/S1028334X17090227
DO - 10.1134/S1028334X17090227
M3 - Article
AN - SCOPUS:85030719874
VL - 476
SP - 1010
EP - 1015
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -
ID: 35813910