Tracing the orogenic sulfur cycle in the Andes using stable isotope composition of dissolved sulfate in thermal springs-Reference-Cited by-同舟云学术

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Tracing the orogenic sulfur cycle in the Andes using stable isotope composition of dissolved sulfate in thermal springs

Published:2024-12 Issue: Volume:669 Page:122365
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Grambling Tyler A.,Newell Dennis L.,Lloyd Karen G.,Hiett Coleman D.,Upin Heather,Barry Peter H.,Giovannelli Donato,de Moor J. Maarten,Chiodi Agostina,Jessen Gerdhard L.,Blamey Jenny M.,Szynkiewicz Anna

Funder

Simons Foundation

National Science Foundation

CONICYT FONDECYT

Alfred P Sloan Foundation

Horizon 2020

Publisher

Elsevier BV

Reference120 articles.

1. Recycling of water, carbon, and sulfur during subduction of serpentinites: a stable isotope study of Cerro del Almirez, Spain;Alt;Earth Planet. Sci. Lett.,2012

2. Sulfur isotopes in plutonic rocks of the great basin as indicators of crustal architecture;Arehart;J. Geol.,2013

3. Dust and aerosols in the Atacama Desert;Arenas-Díaz;Earth Sci. Rev.,2022

4. Coupled tectonic evolution of Andean orogeny and global climate;Armijo;Earth Sci. Rev.,2015

5. Plutonism and the growth of Andean Crust at 9 °S from 100 to 3 Ma;Atherton;J. S. Am. Earth Sci.,1996

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