Geochemical parameters of bottom sediments from the Stromboli Canyon

DOI

In recent sediments of the Stromboli Canyon sides features of mineral and grain size compositions, redox conditions, behavior of Fe, Mn, organic carbon, Mo, and W in an environment of active input of pyroclastic material are considered. Differences in conditions of sedimentation and early diagenesis in the east and west sides of the canyon depending on position of the prevailing direction of drift and steepness of the slopes, as well as types of differentiation of detrital material in sediments under conditions of permanent vibrations are specified.

Supplement to: Pilipchuk, Mikhail F; Golovina, M S; Sokolov, Vassily S (1978): Lithological and geochemical properties of recent sediments from the Stromboli Canyon slopes. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 13(5), 38-51

Identifier
DOI https://doi.org/10.1594/PANGAEA.775942
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.775942
Provenance
Creator Pilipchuk, Mikhail F; Golovina, M S; Sokolov, Vassily S
Publisher PANGAEA
Contributor P.P. Shirshov Institute of Oceanology, Southern Branch
Publication Year 1978
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 2 datasets
Discipline Earth System Research
Spatial Coverage (15.325W, 38.670S, 15.365E, 38.702N); Mediterranean Sea