14C ages, grain size distribution and foraminifer abundance of sediments from the Barents Sea shelf
The origin of friable sediments blanketing the Barents Sea shelf is considered. It is shown that their characteristic seismoacoustic record patterns reflect low degree of diagenetic transformations and indicates continuous sedimentation. According to traditional views, this single sedimentary comple...
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Format: | Dataset |
Language: | English |
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PANGAEA
2009
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.793171 https://doi.org/10.1594/PANGAEA.793171 |