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      Data report: paleomagnetic direction measurements on Expedition 352 igneous core samples

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          Abstract

          Paleomagnetic measurements on International Ocean Discovery Program Expedition 352 basalt samples were undertaken to augment work done on board the R/V JOIDES Resolution during the expedition. A total of 177 new samples were measured using thermal demagnetization experiments with the goal of determining paleomagnetic inclinations from samples for tectonic studies. It was possible to estimate a characteristic remanent magnetization direction from 96% of the measured samples. New data were similar to those of the Expedition reports, with a large range of natural remanent magnetization values and variable demagnetization behaviors, both implying magnetic carriers with a variety of compositions. Paleoinclination values generally matched those found previously, with many having low values indicative of formation near the Equator.

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          Most cited references15

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          The least-squares line and plane and the analysis of palaeomagnetic data

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            Paleomagnetic overprints in ocean sediment cores and their relationship to shear deformation caused by piston coring

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              Self-reversed magnetization carried by titanomaghemite in oceanic basalts

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                Author and article information

                Journal
                10.14379/iodp.proc.352.2015
                Proceedings of the International Ocean Discovery Program
                International Ocean Discovery Program
                2377-3189
                10 April 2018
                Article
                10.14379/iodp.proc.352.202.2018
                4d1380ac-5a38-4841-bb76-afdf6d44dc3e

                This work is licensed under a Creative Commons Attribution 4.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History

                Earth & Environmental sciences,Oceanography & Hydrology,Geophysics,Chemistry,Geosciences

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