Heat Transfer and Production in Cratonic Continental Crust: U‐Pb Thermochronology of Xenoliths From the Siberian Craton-Reference-Cited by-同舟云学术

Heat Transfer and Production in Cratonic Continental Crust: U‐Pb Thermochronology of Xenoliths From the Siberian Craton

Published:2022-10 Issue:10 Volume:23 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Apen Francisco E.¹^ORCID,Rudnick Roberta L.¹,Ionov Dmitri A.²^ORCID,Cottle John M.¹,Moyen Jean‐Franҫois³,Golovin Alexander V.⁴⁵,Korsakov Andrey V.⁴^ORCID

Affiliation:

1. Department of Earth Science and Earth Research Institute University of California, Santa Barbara Santa Barbara CA USA

2. Géosciences Montpellier Université de Montpellier Montpellier France

3. Université Jean‐Monnet Laboratoire Magmas et Volcans UCA‐CNRS‐IRD Aubière France

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

5. Institute of the Earth's Crust Siberian Branch Russian Academy of Sciences Novosibirsk Russia

Funder

National Science Foundation

Russian Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GC010497

Reference138 articles.

1. Metasomatism in lithospheric mantle roots: Constraints from whole-rock and mineral chemical composition of deformed peridotite xenoliths from kimberlite pipe Udachnaya

2. Conservation of deep crustal heat production

3. Isotopic composition (H, O, Cl, Sr) of ground brines of the Siberian Platform

4. Equilibrium-non-equilibrium of the brine-kimberlite system in the Udachnaya pipe, Russia, based on physicochemical modeling

5. The effects of temperature and fO2on the Al-in-hornblende barometer

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