Directional change during a M iocene R ‐ N geomagnetic polarity reversal recorded by mafic lava flows, S heep C reek R ange, north central N evada, USA-Reference-Cited by-同舟云学术

Directional change during a M iocene R ‐ N geomagnetic polarity reversal recorded by mafic lava flows, S heep C reek R ange, north central N evada, USA

Published:2017-09 Issue:9 Volume:18 Page:3470-3488
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Bogue S. W.¹^ORCID,Glen J. M. G.²,Jarboe N. A.³^ORCID

Affiliation:

1. Department of GeologyOccidental CollegeLos Angeles California USA

2. U.S. Geological Survey, MS 989Menlo Park California USA

3. Scripps Institution of Oceanography, University of California San DiegoLa Jolla California USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GC007049

Reference46 articles.

1. Can downwelling at the top of the Earth’s core be detected in the geomagnetic secular variation?

2. Stationary, oscillating or drifting mantle-driven geomagnetic flux patches?

3. Polarity Reversals from Paleomagnetic Observations and Numerical Dynamo Simulations

4. The time-dependence of intense archeomagnetic flux patches

5. The magnetic structure of convection-driven numerical dynamos

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