Using stable isotopes (δ 17 O, δ 18 O and δD) of gypsum hydration water to ascertain the role of water condensation in the formation of subaerial gypsum speleothems-Reference-Cited by-同舟云学术

Using stable isotopes (δ 17 O, δ 18 O and δD) of gypsum hydration water to ascertain the role of water condensation in the formation of subaerial gypsum speleothems

Published:2017-03 Issue: Volume:452 Page:34-46
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Gázquez Fernando^ORCID,Calaforra José María,Evans Nicholas P.,Hodell David A.

Funder

ERC

Junta de Andalucía Regional Government

University of Almería

ECA

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference73 articles.

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