Paleointensity Results From Pliocene Lavas of the Lesser Caucasus Obtained Using the Multispecimen Parallel Differential pTRM Method: A Comparison With Thellier‐Thellier and IZZI Data-Reference-Cited by-同舟云学术

Paleointensity Results From Pliocene Lavas of the Lesser Caucasus Obtained Using the Multispecimen Parallel Differential pTRM Method: A Comparison With Thellier‐Thellier and IZZI Data

Published:2021-04 Issue:4 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Sánchez‐Moreno Elisa M.¹²^ORCID,Calvo‐Rathert Manuel²^ORCID,Goguitchaichvili Avto³,Vashakidze George T.⁴^ORCID,Camps Pierre⁵^ORCID,Morales‐Contreras Juan³^ORCID,Vegas‐Tubía Néstor⁶,Lebedev Vladimir A.⁷

Affiliation:

1. Instituto Dom Luiz (IDL), Faculdade de Ciências Universidade de Lisbon Lisbon Portugal

2. Departamento de Física EPS Campus Rio Vena Universidad de Burgos Burgos Spain

3. Laboratorio Interinstitucional de Magnetismo Natural Instituto de Geofísica Unidad Michoacán UNAM – Campus Morelia Morelia México

4. Alexandre Janelidze Institute of Geology Ivane Javakhishvili Tbilisi State University Tbilisi Georgia

5. Géosciences Montpellier Université de Montpellier CNRS Montpellier France

6. Departamento de Geodinámica Universidad del País Vasco UPV/EHU Leioa Bizkaia Spain

7. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry – Russian Academy of Sciences (IGEM RAS) Moscow Russia

Funder

Consejería de Educación, Junta de Castilla y León

Ministerio de Economía y Competitividad

Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México

Agencia Estatal de Investigación

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/10.1029/2020JB019682

Reference64 articles.

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4. The effect of cooling rate on the intensity of thermoremanent magnetization (TRM) acquired by assemblages of pseudo-single domain, multidomain and interacting single-domain grains

5. A new set of qualitative reliability criteria to aid inferences on paleomagnetic dipole moment variations through geological time;Biggin A. J.;Frontiers of Earth Science,2014

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