Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments
Albian turbidites and intercalated shales were cored from ~1145 to 1700 meters below seafloor at Site 1276 in the Newfoundland Basin. Strata at this level dip ~2.5° seaward (toward an azimuth of ~130°) based on seismic profiles. In contrast, beds dip an average of ~10° in the cores. This higher appa...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2007
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.776586 https://doi.org/10.1594/PANGAEA.776586 |