Macroturbidites of ODP Hole 103-641C
Barremian through uppermost Aptian strata from ODP Hole 641C, located upslope of a tilted fault block on the Galicia margin (northwest Spain), are syn-rift sediments deposited in the bathyal realm and are characterized by rapid sedimentation from turbidity currents and debris flows. Calcarenite and...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1988
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.743869 https://doi.org/10.1594/PANGAEA.743869 |