Using stable isotopes (d 17 O, d 18 O and dD) of gypsum hydration water to ascertain the role of water condensation in the formation of subaerial gypsum speleothems (2017)

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1016/j.chemgeo.2017.01.021

Publication URI: http://dx.doi.org/10.1016/j.chemgeo.2017.01.021

Type: Journal Article/Review

Parent Publication: Chemical Geology