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...

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Bibliographic Details
Main Authors: Faugeres, Jean-Claude, Legigan, Philippe, Maillet, Noelle, Latouche, Claude
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1989
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.746573
https://doi.org/10.1594/PANGAEA.746573