Unmixing detrital zircon U-Pb ages reveals tectonic and climatic depositional influences on the Carboniferous Ansilta Formation, Calingasta-Uspallata Basin, Western Argentina-Reference-Cited by-同舟云学术

Unmixing detrital zircon U-Pb ages reveals tectonic and climatic depositional influences on the Carboniferous Ansilta Formation, Calingasta-Uspallata Basin, Western Argentina

Published:2024-07 Issue:4 Volume:15 Page:101807
ISSN:1674-9871
Container-title:Geoscience Frontiers
language:en
Short-container-title:Geoscience Frontiers

Author:

Malone J.R.,Malone J.E.,Isbell J.L.,Malone D.H.,Craddock J.P.,Pauls K.N.

Funder

National Science Foundation

Publisher

Elsevier BV

Reference186 articles.

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5. El Carbónico marino en el valle Calingasta-Uspallata, San Juan-Mendoza;Amos;Boletin De Informaciones Petroleras,1965

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