Thermochronology and Exhumation History of the Northeastern Fennoscandian Shield Since 1.9 Ga: Evidence From 40 Ar/ 39 Ar and Apatite Fission Track Data From the Kola Peninsula-Reference-Cited by-同舟云学术

Thermochronology and Exhumation History of the Northeastern Fennoscandian Shield Since 1.9 Ga: Evidence From 40 Ar/ 39 Ar and Apatite Fission Track Data From the Kola Peninsula

Published:2019-07 Issue:7 Volume:38 Page:2317-2337
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Veselovskiy Roman V.¹²^ORCID,Thomson Stuart N.³^ORCID,Arzamastsev Andrey A.⁴⁵^ORCID,Botsyun Svetlana⁶^ORCID,Travin Aleksey V.⁷⁸^ORCID,Yudin Denis S.⁷⁸,Samsonov Alexander V.⁹^ORCID,Stepanova Alexandra V.¹⁰^ORCID

Affiliation:

1. Geological FacultyLomonosov Moscow State University Moscow Russia

2. Institute of Physics of the EarthRussian Academy of Sciences Moscow Russia

3. Department of GeosciencesUniversity of Arizona Tucson AZ USA

4. Institute of Precambrian Geology and GeochronologyRussian Academy of Sciences Saint Petersburg Russia

5. Institute of Earth SciencesSaint Petersburg State University Saint Petersburg Russia

6. Department of GeosciencesUniversity of Tuebingen Tuebingen Germany

7. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences Novosibirsk Russia

8. Department of Geology and GeophysicsNovosibirsk State University Novosibirsk Russia

9. Institute of Geology of Ore Deposits Petrography Mineralogy and GeochemistryRussian Academy of Sciences Moscow Russia

10. Institute of Geology, Karelian Research CentreRussian Academy of Sciences Petrozavodsk Russia

Funder

Council on grants of the President of the Russian Federation

Government Council on Grants, Russian Federation

Russian Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005250

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5. Contact interaction of agpaitic magmas with basement gneisses: An example of the Khibina and Lovozero Massifs

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