Chemical composition of the red bed layer in DSDP Hole 38-336

DOI

Clay minerals were studied in samples from the Eocene red bed layer of DSDP Hole 336. It is shown that composition and distribution of clay minerals have zoning, which is usually typical for the terrestrial crust of chemical weathering of basic rocks.

Supplement to: Kharin, Gennady S; Zangalis, K P (1979): Clay minerals of the red beds from the Fareroes-Iceland threshold (North Atlantic). Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 14(3), 31-39

Identifier
DOI https://doi.org/10.1594/PANGAEA.778844
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.778844
Provenance
Creator Kharin, Gennady S; Zangalis, K P
Publisher PANGAEA
Publication Year 1979
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 (-7.788 LON, 63.351 LAT); North Atlantic/Norwegian Sea