Analysis of an Updated Paleointensity Database (Q PI ‐PINT) for 65–200 Ma: Implications for the Long‐Term History of Dipole Moment Through the Mesozoic-Reference-Cited by-同舟云学术

Analysis of an Updated Paleointensity Database (Q PI ‐PINT) for 65–200 Ma: Implications for the Long‐Term History of Dipole Moment Through the Mesozoic

Published:2019-10 Issue:10 Volume:124 Page:9999-10022
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Kulakov E. V.¹^ORCID,Sprain C. J.²³,Doubrovine P. V.¹^ORCID,Smirnov A. V.⁴^ORCID,Paterson G. A.²⁵^ORCID,Hawkins L.²,Fairchild L.⁶^ORCID,Piispa E. J.⁷^ORCID,Biggin A. J.²^ORCID

Affiliation:

1. The Centre for Earth Evolution and Dynamics University of Oslo Oslo Norway

2. Department of Earth, Ocean and Ecological Sciences University of Liverpool Liverpool UK

3. Now at the Department of Geological Sciences University of Florida Gainesville FL USA

4. Department of Geological and Mining Engineering and Sciences and Department of Physics Michigan Technological University Houghton MI USA

5. Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

6. Department of Earth and Planetary Sciences University of California Berkeley CA USA

7. School of Geological Sciences and Engineering Yachay Tech University Ibarra Ecuador

Funder

Natural Environment Research Council

Leverhulme Trust

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB017287

Reference85 articles.

1. Observations and Models of the Long-Term Evolution of Earth’s Magnetic Field

2. A new set of qualitative reliability criteria to aid inferences on palaeomagnetic dipole moment variations through geological time;Biggin A. J.;Frontiers in Earth Sciences,2014

3. Palaeomagnetic field intensity variations suggest Mesoproterozoic inner-core nucleation

4. Possible links between long-term geomagnetic variations and whole-mantle convection processes

5. Evidence for a very-long-term trend in geomagnetic secular variation

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