Geochemical Peculiarities of the Pacific Pleistocene Sediments

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In the geochemical review based on records from cruises of International project of Deep-Sea Drilling and other literature data concerning main lithologic types of the Pacific Pleistocene sediments we presented tables of average arithmetic chemical composition, meanweighted chemical composition, accumulation rates, and mass accumulation rates of chemical components. These tables can be used for comparative analysis with sediments of the same or other stratons in different oceanic basins and also with paleooceanic sediments on the continents. Terrigenous matrix dominates within lithogenic matter. We discovered a close resemblance between chemical composition of hemipelagic clays and volcanic sediments. Peculiarities of hydrothermal sediments are described. Using methods of mathematical statistics, we revealed main geochemical associations and principal factors determinating the chemical composition of studied sediments. Masses of oxides of petrogenic elements and a number of trace elements have been calculated for Pleistocene sediments. We managed to take an idea about average chemical composition of the Pacific Pleistocene.

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M. Levitan

Vernadsky Institute of Geochemistry and Analytical Chemistry of the RAS

编辑信件的主要联系方式.
Email: m-levitan@mail.ru
俄罗斯联邦, 19, Kosygin St., Moscow, 119991

L. Domaratskaya

Vernadsky Institute of Geochemistry and Analytical Chemistry of the RAS

Email: m-levitan@mail.ru
俄罗斯联邦, 19, Kosygin St., Moscow, 119991

A. Koltsova

Vernadsky Institute of Geochemistry and Analytical Chemistry of the RAS

Email: m-levitan@mail.ru
俄罗斯联邦, 19, Kosygin St., Moscow, 119991

K. Syromyatnikov

Vernadsky Institute of Geochemistry and Analytical Chemistry of the RAS

Email: m-levitan@mail.ru
俄罗斯联邦, 19, Kosygin St., Moscow, 119991

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2. Fig. 1. Location of deepwater drilling boreholes in which Pleistocene sediments were characterised by chemical analyses.

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3. Fig. 2. Spider diagram of the chemical composition of Pleistocene sediments in relation to the PAAS composition. 1 - pelagic clays; 2 - hemipelagic clays; 3 - volcanogenic sediments; 4 - hydrothermal sediments; 5 - carbonate-free matter (bqv) of coccolithic silts and clays; 6 - carbonate-free matter (bqv) of coccolithic foraminiferous silts and clays; 7 - diatom silts and clays; 8 - diatom-radiolarian silts and clays.

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4. Fig. 3. Spider diagram of rare earth elements composition in relation to PAAS composition. a - in a number of Pleistocene lithogenic sediments (1 - pelagic clays, 2 - hemipelagic clays, 3 - marine sands, 4 - volcanogenic deposits, 5 - hydrothermal deposits); b - in biogenic sediments (1 - coccolithic muds and clays, 2 - coccolithic-foraminiferal muds and clays, 3 - diatom muds and clays).

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5. Fig. 4. Spider diagram of the chemical composition of Pleistocene sediments in relation to the UCC composition. 1 - terrigenous turbidites; 2 - marine sands; 3 - volcanogenic sediments; 4 - hydrothermal sediments.

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6. Fig. 5. Results of factor analysis.

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7. Fig. 6. Cyclograms of the weighted average chemical composition of Pleistocene sediments (in %). 1 - pelagic clays; 2 - hemipelagic clays; 3 - terrigenous turbidites; 4 - marine sands; 5 - volcanogenic sediments; 6 - coccolithic silts and clays; 7 - coccolithic foraminiferal silts and clays; 8 - diatom muds and clays; 9 - diatom-radiolarian muds and clays; 10 - benthic carbonates and carbonate-clastic sediments; 11 - carbonate turbidites.

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8. Fig. 7. Cyclograms of absolute masses of Pleistocene sediments (in conventional units). 1 - pelagic clays; 2 - hemipelagic clays; 3 - terrigenous turbidites; 4 - volcanogenic-clastic sediments and volcanic ashes; 5 - coccolithic clays and silts; 6 - coccolithic-foraminiferous clays and silts; 7 - benthic and carbonate-clastic sediments; 8 - diatom clays and silts; 9 - diatom-radiolarian clays and silts.

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