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.
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1979
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.778844 https://doi.org/10.1594/PANGAEA.778844 |