Pelagic, turbiditic, and contouritic sequential deposits on the Cape Verde Plateau
On the Cape Verde Plateau, Neogene deposits are composed of major pelagic and hemipelagic sediments. These sediments show climatic sequences composed of two lithologic terms that differ in their siliciclastic and carbonate contents. Several turbiditic and contouritic sequences are interbedded in the...
Main Authors: | , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1989
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.746573 https://doi.org/10.1594/PANGAEA.746573 |