Geochemistry of sediments from the mid-oceanic Kolbeinsey Ridge ...

In order to assess recent submarine volcanic contributions to the sediments from the active Kolbeinsey Ridge, surface samples were analyzed chemically. The contribution of major and trace elements studied differ within the study area.A statistical analysis of the geochemical variables using factor a...

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Bibliographic Details
Main Authors: Lackschewitz, Klas Sven, Wallrabe-Adams, Hans-Joachim, Garbe-Schönberg, Dieter
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1994
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735769
https://doi.pangaea.de/10.1594/PANGAEA.735769
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Summary:In order to assess recent submarine volcanic contributions to the sediments from the active Kolbeinsey Ridge, surface samples were analyzed chemically. The contribution of major and trace elements studied differ within the study area.A statistical analysis of the geochemical variables using factor analysis and cluster method allows to distinguish possible sample groups. Cluster method identifies three distinct sediment groups located in different areas of sedimentation.Group 1 is characterized by highest contents of Fe2O3, V, Co, Ni, Cu and Zn demonstrating the input of volcaniclastic material. Group 2 comprises high values of CaCO3, CaO and Sr representing biogenic carbonate. Group 3 is characterized by the elements K, Rb, Cs, La and Pb indicating the terrigenous component.The absolute percentage of the volcanic, biogenic and terrigenous components in the bulk sediments was calculated by using a normative sediment method. The highest volcanic component (> 60% on a carbonate free basis) is found on the ... : Supplement to: Lackschewitz, Klas Sven; Wallrabe-Adams, Hans-Joachim; Garbe-Schönberg, Dieter (1994): Geochemistry of surface sediments from the mid-oceanic Kolbeinsey Ridge, north of Iceland. Marine Geology, 121(1-2), 105-119 ...