Revealing the mechanisms of soil gypsum formation in the Atacama Desert through triple oxygen and hydrogen isotopes of gypsum hydration water-Reference-Cited by-同舟云学术

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Revealing the mechanisms of soil gypsum formation in the Atacama Desert through triple oxygen and hydrogen isotopes of gypsum hydration water

Published:2024-08 Issue: Volume:243 Page:108171
ISSN:0341-8162
Container-title:CATENA
language:en
Short-container-title:CATENA

Author:

Gázquez Fernando^ORCID,Voigt Claudia,Claire Mark W.^ORCID,Rull Fernando,Medina Jesús^ORCID,Hodell David A.^ORCID

Publisher

Elsevier BV

Reference72 articles.

1. Iodine budget in surface waters from Atacama: natural and anthropogenic iodine sources revealed by halogen geochemistry and iodine isotopes;Álvarez;Appl. Geochem.,2016

2. Coastal fog and its relation to groundwater in the IV region of northern Chile;Aravena;Chem. Geol.,1989

3. Sequence stratigraphy of the Mesozoic Domeyko Basin, northern Chile;Ardill;J. Geol. Soc. London,1998

4. 0.3 byr of drainage stability along the Palaeozoic palaeo-Pacific Gondwana margin; a detrital zircon study;Augustsson;J. Geol. Soc. London,2015

5. Unprecedented rains decimate surface microbial communities in the hyperarid core of the Atacama Desert;Azua-Bustos;Sci. Rep.,2018

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