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Structure of hydrothermal aureoles in the Pacific and Atlantic Oceans. / Sudarikov, S. M.; Cherkashev, G. A.

In: Transactions - Doklady, Russian Academy of Sciences: Earth Science, Vol. 331, No. 5, 01.01.1993, p. 217-221.

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Harvard

Sudarikov, SM & Cherkashev, GA 1993, 'Structure of hydrothermal aureoles in the Pacific and Atlantic Oceans', Transactions - Doklady, Russian Academy of Sciences: Earth Science, vol. 331, no. 5, pp. 217-221.

APA

Sudarikov, S. M., & Cherkashev, G. A. (1993). Structure of hydrothermal aureoles in the Pacific and Atlantic Oceans. Transactions - Doklady, Russian Academy of Sciences: Earth Science, 331(5), 217-221.

Vancouver

Sudarikov SM, Cherkashev GA. Structure of hydrothermal aureoles in the Pacific and Atlantic Oceans. Transactions - Doklady, Russian Academy of Sciences: Earth Science. 1993 Jan 1;331(5):217-221.

Author

Sudarikov, S. M. ; Cherkashev, G. A. / Structure of hydrothermal aureoles in the Pacific and Atlantic Oceans. In: Transactions - Doklady, Russian Academy of Sciences: Earth Science. 1993 ; Vol. 331, No. 5. pp. 217-221.

BibTeX

@article{5a83d552a4374e2eb1acbcff97412df2,
title = "Structure of hydrothermal aureoles in the Pacific and Atlantic Oceans",
abstract = "The correlations between the well-defined components of the compositions of the hydrothermal solutions (their end members) was examined. A principal group of elements is distinguished that have persistent positive correlations, both quantitatively and qualitatively: Cl-Na-Ca-Mn-Fe-Zn. The elements in the set determine the compositions and geochemical features of the hydrothermal solutions as regards the macroscopic and microscopic compositions, while the triad of trace components (Mn, Fe, and Zn) is the leading feature in the geochemical pattern of the hydrothermal plumes. It is thought that the main role is played by dissolved forms of Mn and suspended forms of Fe while the black smoke from the smokers consists mainly of Fe sulfides and hydroxides. -from Journal translation",
author = "Sudarikov, {S. M.} and Cherkashev, {G. A.}",
year = "1993",
month = jan,
day = "1",
language = "English",
volume = "331",
pages = "217--221",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Structure of hydrothermal aureoles in the Pacific and Atlantic Oceans

AU - Sudarikov, S. M.

AU - Cherkashev, G. A.

PY - 1993/1/1

Y1 - 1993/1/1

N2 - The correlations between the well-defined components of the compositions of the hydrothermal solutions (their end members) was examined. A principal group of elements is distinguished that have persistent positive correlations, both quantitatively and qualitatively: Cl-Na-Ca-Mn-Fe-Zn. The elements in the set determine the compositions and geochemical features of the hydrothermal solutions as regards the macroscopic and microscopic compositions, while the triad of trace components (Mn, Fe, and Zn) is the leading feature in the geochemical pattern of the hydrothermal plumes. It is thought that the main role is played by dissolved forms of Mn and suspended forms of Fe while the black smoke from the smokers consists mainly of Fe sulfides and hydroxides. -from Journal translation

AB - The correlations between the well-defined components of the compositions of the hydrothermal solutions (their end members) was examined. A principal group of elements is distinguished that have persistent positive correlations, both quantitatively and qualitatively: Cl-Na-Ca-Mn-Fe-Zn. The elements in the set determine the compositions and geochemical features of the hydrothermal solutions as regards the macroscopic and microscopic compositions, while the triad of trace components (Mn, Fe, and Zn) is the leading feature in the geochemical pattern of the hydrothermal plumes. It is thought that the main role is played by dissolved forms of Mn and suspended forms of Fe while the black smoke from the smokers consists mainly of Fe sulfides and hydroxides. -from Journal translation

UR - http://www.scopus.com/inward/record.url?scp=0027900315&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0027900315

VL - 331

SP - 217

EP - 221

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 5

ER -

ID: 35878215