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  1. Book ; Online: Mineral and chemical compositions of carbonates from the Lost Village hydrothermal field, Mid-Atlantic Ridge, supplementary data to: Dara, OM; Kuz'mina, Tatyana G; Lein, Alla Yu (2009): Mineral Associations of the Lost Village and Lost City hydrothermal fields in the North Atlantic. Translated from Okeanologiya, 2009, 49(5), 742-750, Oceanology, 49(5), 688-696

    Dara, OM / Kuz'mina, Tatyana G / Lein, Alla Yu

    2009  

    Abstract: During Cruise 50 of R/V Akademik Mstislav Keldysh on the south slope of the Atlantis massif (30°07'N, Middle Atlantic Ridge) an inactive hydrothermal field named Lost Village was discovered. This new field was composed of light carbonate rock and was ... ...

    Abstract During Cruise 50 of R/V Akademik Mstislav Keldysh on the south slope of the Atlantis massif (30°07'N, Middle Atlantic Ridge) an inactive hydrothermal field named Lost Village was discovered. This new field was composed of light carbonate rock and was located near the active Lost City hydrothermal field. Mineral associations of these fields were studied. A conclusion about participation of ocean water in changing of carbonate composition of the inactive hydrothermal field was made.
    Language English
    Dates of publication 2009-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Online
    Note This dataset is supplement to doi:10.1134/S0001437009050105
    DOI 10.1594/PANGAEA.767383
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  2. Book ; Online: Chemical composition of surface layer bottom sediments from the White Sea collected in Cruises 49 and 80 of R/V Professor Shtockman, supplementary data to: Kuz'mina, Tatyana G; Lein, Alla Yu; Luchsheva, LN; Murdmaa, Ivar O; Novigatsky, Alexander N; Shevchenko, Vladimir P (2009): Chemical composition of surface sediments of the White Sea. Translated from Litologiya i Poleznyye Iskopaemyye, 2009, 44(2), 115-132, Lithology and Mineral Resources, 44(2), 103-119

    Kuz'mina, Tatyana G / Lein, Alla Yu / Luchsheva, LN / Murdmaa, Ivar O / Novigatsky, Alexander N / Shevchenko, Vladimir P

    2009  

    Abstract: Contents of major elements in surface layer bottom sediments of the White Sea were determined by the X-ray fluorescence method. Application of the statistical analysis (principal component method and cluster analysis) made it possible to divide the ... ...

    Abstract Contents of major elements in surface layer bottom sediments of the White Sea were determined by the X-ray fluorescence method. Application of the statistical analysis (principal component method and cluster analysis) made it possible to divide the sediments into more or less homogeneous seven groups with different chemical and grain size compositions. In general, the groups corresponded to sediment lithotypes based on the P.P. Shirshov Institute of Oceanology classification. Contents of Si and Al are controlled by sand-silt and pelite fraction ratio, while variations in Mn (and Fe in part) content are governed by redistribution of elements during redox processes of early diagenesis.
    Language English
    Dates of publication 2009-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Online
    Note This dataset is supplement to doi:10.1134/S0024490209020011
    DOI 10.1594/PANGAEA.777351
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  3. Book ; Online: Chemical composition of White Sea bottom sediments, supplementary data to: Kuz'mina, Tatyana G; Lein, Alla Yu; Luchsheva, LN; Murdmaa, Ivar O; Novigatsky, Alexander N; Shevchenko, Vladimir P (2009): Chemical composition of surface sediments of the White Sea. Translated from Litologiya i Poleznyye Iskopaemyye, 2009, 44(2), 115-132, Lithology and Mineral Resources, 44(2), 103-119

    Kuz'mina, Tatyana G / Lein, Alla Yu / Luchsheva, LN / Murdmaa, Ivar O / Novigatsky, Alexander N / P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, @Moscow / Shevchenko, Vladimir P

    2009  

    Abstract: Contents of major elements in surface layer bottom sediments of the White Sea were determined by the X-ray fluorescence method. Application of the statistical analysis (principal component method and cluster analysis) made it possible to divide the ... ...

    Abstract Contents of major elements in surface layer bottom sediments of the White Sea were determined by the X-ray fluorescence method. Application of the statistical analysis (principal component method and cluster analysis) made it possible to divide the sediments into more or less homogeneous seven groups with different chemical and grain size compositions. In general, the groups corresponded to sediment lithotypes based on the classification elaborated at P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences. Contents of Si and Al are controlled by the ratio of sand-silt and pelite grain size fractions, while variations in content of Mn (and Fe in part) are governed by redistribution of elements in the course of redox processes of early diagenesis.
    Language English
    Dates of publication 2009-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Online
    Note This dataset is supplement to doi:10.1134/S0024490209020011
    DOI 10.1594/PANGAEA.787183
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  4. Book ; Online: Mineral and chemical compositions of sedimentary and volcano-sedimentary rocks drilled in DSDP Legs 43 and 44, supplementary data to: Murdmaa, Ivar O; Bazilevskaya, Elena S; Gordeev, Vyacheslav V; Emelyanov, Emelyan M; Kazakova, Vera P; Kuz'mina, Tatyana G; Mukhina, Valentina V; Rudakova, Alevtina N; Turanskaya, Natalya V (1979): Geological Formations of the Southwest Atlantic Ocean. Bezrukov, P.L. (Ed.), Nauka Publ. (Moscow): in Russian, 207 pp

    Murdmaa, Ivar O / Bazilevskaya, Elena S / Emelyanov, Emelyan M / Gordeev, Vyacheslav V / Kazakova, Vera P / Kuz'mina, Tatyana G / Mukhina, Valentina V / Rudakova, Alevtina N / Turanskaya, Natalya V

    1979  

    Abstract: Sedimentary cover on the bottom of the Northwest Atlantic Ocean is underlain by Late Jurassic - Cretaceous tholeiite-basalt formation. It consists of come sedimentary formations with different lithologic features and age. Their composition, stratigraphic ...

    Abstract Sedimentary cover on the bottom of the Northwest Atlantic Ocean is underlain by Late Jurassic - Cretaceous tholeiite-basalt formation. It consists of come sedimentary formations with different lithologic features and age. Their composition, stratigraphic position and, distribution are described on materials of deep-sea drilling. Mineralogical and geochemical studies of DSDP Leg 43 and Leg 44 holes lead to new ideas about composition and genesis of some sediment types of and their associations. High metal contents in the chalk formation of black clays on the Bermuda Rise probably result from exhalations. Connection of red-colored and speckled deposits with hiatuses in sedimentation is shown. Main stages of geological history of the North American Basin are reflected in accumulation of the followed formations: ancient carbonate formation (Late Jurassic - Early Cretaceous), formation of black clays rich in organic matter (Cretaceous), formation of speckled clays (Late Cretaceous), siliceous-clayey turbidite formation (Eocene), hemipelagic and pelagic clayey formation (Neogene), and terrigenous turbidite formation (Pleistocene).
    Language English
    Dates of publication 1979-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Online
    DOI 10.1594/PANGAEA.733319
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  5. Book ; Online: Chemical and mineral compositions of recent and ancient sediments and sedimentary rocks from the Mariana Trench, supplementary data to: Skornyakova, Nadezhda S; Gorbunova, Zinaida N; Kruglikova, Svetlana B; Kuz'mina, Tatyana G; Rudakova, Alevtina N; Ushakova, Maola G (1978): Sediments and sedimentary rocks from the Mariana Trench. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 13(5), 18-32

    Skornyakova, Nadezhda S / Gorbunova, Zinaida N / Kruglikova, Svetlana B / Kuz'mina, Tatyana G / Moscow, P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences / Rudakova, Alevtina N / Ushakova, Maola G

    1978  

    Abstract: On the bed and on the ocean slope of the southern latitudinal part of the Mariana Trench ancient sediments, as well as sedimentary and igneous rocks are exposed. In the lower part of the sampled part of the studied section Late Oligocene to Early Miocene ...

    Abstract On the bed and on the ocean slope of the southern latitudinal part of the Mariana Trench ancient sediments, as well as sedimentary and igneous rocks are exposed. In the lower part of the sampled part of the studied section Late Oligocene to Early Miocene chalk-like limestones and marls occur. Upward marly tuffites and tuffs (apparently alternating with carbonate rocks) occur. These rocks are overlain by Early Miocene tuffaceous clays and siliceous-clayey muds. In the upper part of the section there are Pleistocene pelagic clays and ethmodiscus oozes.
    Language English
    Dates of publication 1978-9999
    Size Online-Ressource
    Publisher PANGAEA - Data Publisher for Earth & Environmental Science
    Publishing place Bremen/Bremerhaven
    Document type Book ; Online
    DOI 10.1594/PANGAEA.775929
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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