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

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: Dataset
Language:English
Published: PANGAEA 1979
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.778844
https://doi.org/10.1594/PANGAEA.778844