Geochemistry of Neogene-Quaternary sediments in ODP Site 105-645

Subcontinuously cored early(?)-middle Miocene to recently deposited sediments from ODP Site 645 were studied texturally, mineralogically, and geochemically. The entire sequence contains minerals and associated chemical elements that are chiefly of detrital origin. In particular, the clay minerals, w...

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Bibliographic Details
Main Authors: ThiƩbault, Francois, Cremer, Michel, Debrabant, Pierre, Foulon, J, Nielsen, Ole Bjorslev, Zimmerman, Herman
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1989
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.745176
https://doi.org/10.1594/PANGAEA.745176