(Table 1) Detrital modes for sand grains in sediment core CRP-2/2A
Dynamic provenance variations are deduced from sand-grain detrital modes in samples obtained from the CRP-2/2A drillcore. Below an important unconformity at 307 metres below sea floor (mbsf), sand grains in most of the sequence were dominantly derived from Beacon sandstone and Ferra dolerite sources...
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Format: | Dataset |
Language: | English |
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PANGAEA
2000
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.191104 https://doi.org/10.1594/PANGAEA.191104 |