Paleomagnetic analysis of the Oligocene to early Miocene sediments of IODP SIte 342-U1406

Fine-grained magnetic particles in deep-sea sediments often statistically align with the ambient magnetic field during (and shortly after) deposition and can therefore record geomagnetic reversals. Correlation of these reversals to a geomagnetic polarity time scale is an important geochronological t...

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Bibliographic Details
Main Authors: van Peer, Tim E, Xuan, Chuang, Lippert, Peter C, Liebrand, Diederik, Agnini, Claudia, Wilson, Paul A
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.880978
https://doi.org/10.1594/PANGAEA.880978