Late pleistocene and holocene sedimentation in the central and eastern Persian Gulf
The sandfraction of the sediment was analysed in five cores, taken from 65 m water depth in the central and eastern part of the Persian Gulf. The holocene marls are underlayn by aragonite muds, which are probably 10-11,000 years old. 1. The cores could be subdivided into coarse grained and fine grai...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1972
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.548411 https://doi.org/10.1594/PANGAEA.548411 |