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New hydrothermal field at the axial zone of the mid-Atlantic ridge. / Bel'tenev, V. E.; Neshcheretov, A. V.; Ivanov, V. N.; Shilov, V. V.; Rozhdestvenskaya, I.I.; Shagin, A. A.; Stepanova, T. V.; Andreeva, I. A.; Semenov, Yu P.; Sergeev, M. B.; Cherkashev, G. A.; Batuev, B. N.; Samovarov, M. L.; Krotov, A. G.; Markov, V. F.

в: Doklady Akademii Nauk, Том 397, № 1, 21.12.2004, стр. 78-82.

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

Harvard

Bel'tenev, VE, Neshcheretov, AV, Ivanov, VN, Shilov, VV, Rozhdestvenskaya, II, Shagin, AA, Stepanova, TV, Andreeva, IA, Semenov, YP, Sergeev, MB, Cherkashev, GA, Batuev, BN, Samovarov, ML, Krotov, AG & Markov, VF 2004, 'New hydrothermal field at the axial zone of the mid-Atlantic ridge', Doklady Akademii Nauk, Том. 397, № 1, стр. 78-82.

APA

Bel'tenev, V. E., Neshcheretov, A. V., Ivanov, V. N., Shilov, V. V., Rozhdestvenskaya, I. I., Shagin, A. A., Stepanova, T. V., Andreeva, I. A., Semenov, Y. P., Sergeev, M. B., Cherkashev, G. A., Batuev, B. N., Samovarov, M. L., Krotov, A. G., & Markov, V. F. (2004). New hydrothermal field at the axial zone of the mid-Atlantic ridge. Doklady Akademii Nauk, 397(1), 78-82.

Vancouver

Bel'tenev VE, Neshcheretov AV, Ivanov VN, Shilov VV, Rozhdestvenskaya II, Shagin AA и пр. New hydrothermal field at the axial zone of the mid-Atlantic ridge. Doklady Akademii Nauk. 2004 Дек. 21;397(1):78-82.

Author

Bel'tenev, V. E. ; Neshcheretov, A. V. ; Ivanov, V. N. ; Shilov, V. V. ; Rozhdestvenskaya, I.I. ; Shagin, A. A. ; Stepanova, T. V. ; Andreeva, I. A. ; Semenov, Yu P. ; Sergeev, M. B. ; Cherkashev, G. A. ; Batuev, B. N. ; Samovarov, M. L. ; Krotov, A. G. ; Markov, V. F. / New hydrothermal field at the axial zone of the mid-Atlantic ridge. в: Doklady Akademii Nauk. 2004 ; Том 397, № 1. стр. 78-82.

BibTeX

@article{9c45dc15a3994759ac89e23e49315644,
title = "New hydrothermal field at the axial zone of the mid-Atlantic ridge",
abstract = "It is established that the new (discovered in 2003) active hydrothermal ore field is located on the surface of tectonic terrace at the foot of rift valley western bank in the region of edge plutonic fracture intersection with the zone of sub-latitudinal tectonic deformations. The hydrothermal field is the first one discovered in the western bank of rift valley, the 'deepest' in Atlantic Ocean and the third of associated with plutonic rocks of the gabbro-peridotite complex. The preliminary data indicate differentiated, long-term and complex character of ore-formation process, which manifests in the zonal structure of ore bodies.",
author = "Bel'tenev, {V. E.} and Neshcheretov, {A. V.} and Ivanov, {V. N.} and Shilov, {V. V.} and I.I. Rozhdestvenskaya and Shagin, {A. A.} and Stepanova, {T. V.} and Andreeva, {I. A.} and Semenov, {Yu P.} and Sergeev, {M. B.} and Cherkashev, {G. A.} and Batuev, {B. N.} and Samovarov, {M. L.} and Krotov, {A. G.} and Markov, {V. F.}",
year = "2004",
month = dec,
day = "21",
language = "English",
volume = "397",
pages = "78--82",
journal = "ДОКЛАДЫ АКАДЕМИИ НАУК",
issn = "0869-5652",
publisher = "Издательство {"}Наука{"}",
number = "1",

}

RIS

TY - JOUR

T1 - New hydrothermal field at the axial zone of the mid-Atlantic ridge

AU - Bel'tenev, V. E.

AU - Neshcheretov, A. V.

AU - Ivanov, V. N.

AU - Shilov, V. V.

AU - Rozhdestvenskaya, I.I.

AU - Shagin, A. A.

AU - Stepanova, T. V.

AU - Andreeva, I. A.

AU - Semenov, Yu P.

AU - Sergeev, M. B.

AU - Cherkashev, G. A.

AU - Batuev, B. N.

AU - Samovarov, M. L.

AU - Krotov, A. G.

AU - Markov, V. F.

PY - 2004/12/21

Y1 - 2004/12/21

N2 - It is established that the new (discovered in 2003) active hydrothermal ore field is located on the surface of tectonic terrace at the foot of rift valley western bank in the region of edge plutonic fracture intersection with the zone of sub-latitudinal tectonic deformations. The hydrothermal field is the first one discovered in the western bank of rift valley, the 'deepest' in Atlantic Ocean and the third of associated with plutonic rocks of the gabbro-peridotite complex. The preliminary data indicate differentiated, long-term and complex character of ore-formation process, which manifests in the zonal structure of ore bodies.

AB - It is established that the new (discovered in 2003) active hydrothermal ore field is located on the surface of tectonic terrace at the foot of rift valley western bank in the region of edge plutonic fracture intersection with the zone of sub-latitudinal tectonic deformations. The hydrothermal field is the first one discovered in the western bank of rift valley, the 'deepest' in Atlantic Ocean and the third of associated with plutonic rocks of the gabbro-peridotite complex. The preliminary data indicate differentiated, long-term and complex character of ore-formation process, which manifests in the zonal structure of ore bodies.

UR - http://www.scopus.com/inward/record.url?scp=10144227792&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:10144227792

VL - 397

SP - 78

EP - 82

JO - ДОКЛАДЫ АКАДЕМИИ НАУК

JF - ДОКЛАДЫ АКАДЕМИИ НАУК

SN - 0869-5652

IS - 1

ER -

ID: 35831269