Planktonic foraminifera of ODP Hole 107-654A ...
The late Miocene sediments of the Tyrrhenian ODP Site 654 encompass a deepening sequence which begins with glauconite shallow water sands followed by a rapid transition to deep water sediments and culminates with dolomitic mudstones associated with Messinian evaporites. The sequence compares well wi...
Main Authors: | , , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
1990
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.744011 https://doi.pangaea.de/10.1594/PANGAEA.744011 |