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...

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Bibliographic Details
Main Authors: Haggerty, Janet A, Germann, Scott H
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1988
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.743869
https://doi.org/10.1594/PANGAEA.743869