Structure, Materials and Processes in the Earth’s Core and Mantle

Véronique Dehant*, Saioa A. Campuzano, Angelo De Santis, Wim van Westrenen

*Corresponding author for this work

Research output: Contribution to JournalReview articleAcademicpeer-review

Abstract

Abstract: This paper reviews current knowledge about the Earth’s core and the overlying deep mantle in terms of structure, chemical and mineralogical compositions, physical properties, and dynamics, using information from seismology, geophysics, and geochemistry. High-pressure experimental techniques that can help to interpret and understand observations of these properties and compositions in the deep interior are summarized. The paper also examines the consequences of core flows on global observations such as variations in Earth’s rotation and orientation or variations in the Earth’s magnetic field. Processes currently active at the core-mantle boundary and the various coupling mechanisms between the core and the mantle are discussed, together with some evidence from magnetic field observations.

Original languageEnglish
Pages (from-to)263-302
Number of pages40
JournalSurveys in Geophysics
Volume43
Issue number1
Early online date1 Feb 2022
DOIs
Publication statusPublished - Feb 2022

Bibliographical note

Funding Information:
R.G. Tr?nnes wrote some of the original text but decided to refrain from co-authorship. We would like to thank him for his contribution. V. Dehant has received funding from the European Research Council (ERC) under the European Union?s Horizon 2020 research and innovation program (GRACEFUL Synergy Grant Agreement No. 855677). W. van Westrenen acknowledges funding through a Netherlands Science Organization (N.W.O.) Vici grant. S. A. Campuzano acknowledges the Juan de la Cierva Formaci?n Program (FJC2018-037643-I). A. De Santis acknowledges funding from Pianeta Dinamico-Working Earth project. All the authors would like to thank ISSI for organizing the ?Probing the Earth?s Deep Interior Using in Synergy Observations of the Earth?s Gravity and Magnetic Fields, and of the Earth?s Rotation? meeting in these challenging times. Last but not least, the authors want to deeply thank S-I. Karato and an anonymous reviewer for helpful comments.

Funding Information:
R.G. Trønnes wrote some of the original text but decided to refrain from co-authorship. We would like to thank him for his contribution. V. Dehant has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (GRACEFUL Synergy Grant Agreement No. 855677). W. van Westrenen acknowledges funding through a Netherlands Science Organization (N.W.O.) Vici grant. S. A. Campuzano acknowledges the Juan de la Cierva Formación Program (FJC2018-037643-I). A. De Santis acknowledges funding from Pianeta Dinamico-Working Earth project. All the authors would like to thank ISSI for organizing the “Probing the Earth’s Deep Interior Using in Synergy Observations of the Earth’s Gravity and Magnetic Fields, and of the Earth’s Rotation” meeting in these challenging times. Last but not least, the authors want to deeply thank S-I. Karato and an anonymous reviewer for helpful comments.

Publisher Copyright:
© 2022, The Author(s).

Funding

R.G. Trønnes wrote some of the original text but decided to refrain from co-authorship. We would like to thank him for his contribution. V. Dehant has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (GRACEFUL Synergy Grant Agreement No. 855677). W. van Westrenen acknowledges funding through a Netherlands Science Organization (N.W.O.) Vici grant. S. A. Campuzano acknowledges the Juan de la Cierva Formación Program (FJC2018-037643-I). A. De Santis acknowledges funding from Pianeta Dinamico-Working Earth project. All the authors would like to thank ISSI for organizing the “Probing the Earth’s Deep Interior Using in Synergy Observations of the Earth’s Gravity and Magnetic Fields, and of the Earth’s Rotation” meeting in these challenging times. Last but not least, the authors want to deeply thank S-I. Karato and an anonymous reviewer for helpful comments. R.G. Trønnes wrote some of the original text but decided to refrain from co-authorship. We would like to thank him for his contribution. V. Dehant has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (GRACEFUL Synergy Grant Agreement No. 855677). W. van Westrenen acknowledges funding through a Netherlands Science Organization (N.W.O.) Vici grant. S. A. Campuzano acknowledges the Juan de la Cierva Formación Program (FJC2018-037643-I). A. De Santis acknowledges funding from Pianeta Dinamico-Working Earth project. All the authors would like to thank ISSI for organizing the “Probing the Earth’s Deep Interior Using in Synergy Observations of the Earth’s Gravity and Magnetic Fields, and of the Earth’s Rotation” meeting in these challenging times. Last but not least, the authors want to deeply thank S-I. Karato and an anonymous reviewer for helpful comments.

FundersFunder number
ISSI
Juan de la Cierva Formación ProgramFJC2018-037643-I
Netherlands Science Organization
Horizon 2020 Framework Programme855677
European Research Council
Nederlandse Organisatie voor Wetenschappelijk Onderzoek

    Keywords

    • Earth’s core
    • Earth’s magnetic field
    • Earth’s rotation
    • Interior structure

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