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Revised geomagnetic polarity time scale for the interval 0–5 m.y. B.P.

Mankinen, Edward A., Dalrymple, G. Brent·1979·Journal of Geophysical Research: Solid Earth

Abstract

A change in the constants used in K‐Ar dating and a significant increase in new data have made a recompilation and recomputation of data used to define the Late Cenozoic K‐Ar polarity time scale highly desirable at this time. All available data in the range 0–5 m.y. have been recalculated using the refined constants, with 354 data points in this time interval now meeting the minimum criteria for acceptability. Recalculation of the major polarity epoch boundaries has yielded ages of 0.73 m.y. for the Brunhes‐Matuyama, 2.48 m.y. for the Matuyama‐Gauss, and 3.40 m.y. for the Gauss‐Gilbert boundaries. A revised polarity time scale has been constructed based on available K‐Ar data and information obtained from marine magnetic anomalies and deep‐sea sedimentary cores.

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Metadata

Authors
Mankinen, E. A., & Dalrymple, G. B.
Venue
Journal of Geophysical Research: Solid Earth
Published
1979-02-10
Volume
84
Issue
B2
Pages
615-626
ISSN
0148-0227 (ISSN-L)
OpenAlex
W1999012927
Cited by
570
References
0
FWCI
15.83
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Revised geomagnetic polarity time scale for the interval 0–5 m.y. B.P. https://app.cochat.ai/papers/10.1029/jb084ib02p00615
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Mankinen, E. A., & Dalrymple, G. B. (1979). Revised geomagnetic polarity time scale for the interval 0–5 m.y. B.P. Journal of Geophysical Research: Solid Earth. https://doi.org/10.1029/jb084ib02p00615

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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