Initial Stage of the Hydrothermal Ore Accumulation within the Field at 9 deg 50' N on the East Pacific Rise

Yu.A.Bogdanov; A.Yu.Lein; A.A.Ulyanov; V.V.Maslennikov; N.V.Ulyanova; A.M.Sagalevich

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Initial Stage of the Hydrothermal Ore Accumulation within the Field at 9 deg 50' N on the East Pacific Rise

机译：东太平洋上升沿9度50'N时田内热液成矿的初始阶段

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In 2003,several hydrothermal mounds located at 9 deg 50' N on the East Pacific Rise were described and sampled during the expedition of R/V Akademik Mstislav Keldysh during dives of Mir deep-sea manned submersibles.These hydrothermal mounds were formed during a few recent years after the volcanic activity in this region that occurred in 1991.The studies of the chemical and mineralogical compositions of the hydrothermal deposits of these mounds and of the chemical composition of the principal sulfide minerals helped to describe the initial stage of the formation of the hydrothermal circulation system and the initiation of the hydro-thermal ore formation.

机译：2003年，在米尔（Mir）深海载人潜水器潜水期间，R / V Akademik Mstislav Keldysh考察期间描述并采样了东太平洋上升沿9度50'N处的几个热液丘。 1991年该地区发生火山活动之后的最近几年。对这些土墩的热液沉积物的化学和矿物组成以及主要硫化物矿物的化学组成的研究有助于描述该火山形成的初始阶段。热液循环系统和热液成矿的开始。

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《Oceanology》 |2006年第1期|共14页
作者
Yu.A.Bogdanov; A.Yu.Lein; A.A.Ulyanov; V.V.Maslennikov; N.V.Ulyanova; A.M.Sagalevich;
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1. Initial Stage of the Hydrothermal Ore Accumulation within the Field at 9 deg 50' N on the East Pacific Rise [J] . Yu.A.Bogdanov, A.Yu.Lein, A.A.Ulyanov, Oceanology . 2006,第1期

机译：东太平洋上升沿9度50'N时田内热液成矿的初始阶段
2. Geochemistry of the Metalliferous Sediments of Hydrothermal Fields of the East Pacific Rise, 11deg30'-13deg N. Part 1. Geochemistry of Holocene Sediments [J] . M. P. Davydov, S. M. Sudarikov, P. A. Aleksandrov, Geochemistry International . 2002,第3期

机译：东太平洋以北11deg30'-13deg的热液含金属沉积物的地球化学。第1部分。全新世沉积物的地球化学
3. Lipids in Hydrothermal Sulfide Ores from the 9°50′N Field of the East Pacific Rise [J] . A. Yu. Lein, V. I. Peresypkin, Yu. A. Bogdanov, Doklady Earth Sciences . 2005,第8期

机译：东太平洋上升9°50′N场热液硫化矿中的脂质
4. Resource Potential of Hydrothermal Activity on the East Pacific Rise (8 deg N - 14 deg N) [C] . N. Okamoto, Y. Matsuura ISOPE ocean mining symposium . 1995

机译：东太平洋崛起水热活动的资源潜力（8° - 14°D）
5. Time-series electrochemical studies in the lower Delaware Bay and at the 9 degrees 50' north East Pacific Rise hydrothermal vent field. [D] . Moore, Tommy S. 2008

机译：在特拉华湾下部和东太平洋上升北坡9度50'热液喷口处进行的时间序列电化学研究。
6. Diversity of Meiofauna from the 9°50′N East Pacific Rise across a Gradient of Hydrothermal Fluid Emissions [O] . Sabine Gollner, Barbara Riemer, Pedro Martínez Arbizu, 2010

机译：东太平洋上升9°50N以来热液流体排放梯度中的Meiofauna多样性
7. Dissolved organic carbon compounds in deep-sea hydrothermal vent fluids from the East Pacific Rise at 9°50′N [O] . Krista Longnecker, Stefan M. Sievert, Sean P. Sylva, 2018

机译：来自东太平洋深海水热通风液中的溶解有机碳化合物在9°50'N的9°
8. Joint Sea Beam/SeaMARC II Survey of the East Pacific Rise and Its Flanks 7 deg 50min-10 deg 30 min N, to Establish a Geologic Acoustic Natural Laboratory [R] . MacDonald, K. C. 1991

机译：联合海梁/ seamaRC II东太平洋上升及其侧翼调查7度50分-10秒30分N，建立地质声学自然实验室

Initial Stage of the Hydrothermal Ore Accumulation within the Field at 9 deg 50' N on the East Pacific Rise

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