A Late Cretaceous‐Eocene Geomagnetic Polarity Timescale (MQSD20) That Steadies Spreading Rates on Multiple Mid‐Ocean Ridge Flanks

A. Malinverno; K. Quigley; A. Staro; J. Dyment

doi:10.1029/2020JB020034

Journal Articles Journal of Geophysical Research : Solid Earth Year : 2020

A Late Cretaceous‐Eocene Geomagnetic Polarity Timescale (MQSD20) That Steadies Spreading Rates on Multiple Mid‐Ocean Ridge Flanks

(1) , (2) , , (3)

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A. Malinverno

Function : Author

Lamont-Doherty Earth Observatory

K. Quigley

Function : Author

Brown University, Providence, Rhode Island

A. Staro

Function : Author

J. Dyment

Function : Author
PersonId : 180159
IdHAL : jerome-dyment
ORCID : 0000-0002-7677-0541
IdRef : 114443173

Institut de Physique du Globe de Paris

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Geophysics [physics.geo-ph]

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2020JB020034(1).pdf (6.76 Mo)

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Jérôme Dyment : Connect in order to contact the contributor

https://hal-insu.archives-ouvertes.fr/insu-03066214

Submitted on : Tuesday, December 15, 2020-10:42:54 AM

Last modification on : Monday, May 1, 2023-3:45:43 AM

Long-term archiving on: Tuesday, March 16, 2021-7:09:01 PM

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insu-03066214 , version 1 (15-12-2020)

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HAL Id : insu-03066214 , version 1
DOI : 10.1029/2020JB020034

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A. Malinverno, K. Quigley, A. Staro, J. Dyment. A Late Cretaceous‐Eocene Geomagnetic Polarity Timescale (MQSD20) That Steadies Spreading Rates on Multiple Mid‐Ocean Ridge Flanks. Journal of Geophysical Research : Solid Earth, 2020, 125 (8), ⟨10.1029/2020JB020034⟩. ⟨insu-03066214⟩

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A Late Cretaceous‐Eocene Geomagnetic Polarity Timescale (MQSD20) That Steadies Spreading Rates on Multiple Mid‐Ocean Ridge Flanks

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