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

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.

Bibliographic Details
Main Authors: Kharin, Gennady S, Zangalis, K P
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1979
Subjects:
Drilling/drill rig
Leg38
Glomar Challenger
Archive of Ocean Data ARCOD
Deep Sea Drilling Project DSDP
Iceland
North Atlantic
Online Access:https://dx.doi.org/10.1594/pangaea.778844
https://doi.pangaea.de/10.1594/PANGAEA.778844
Description
Summary: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.

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