Using stable isotopes (d17O, d18O and dD) of gypsum hydration water to ascertain the role of water condensation in the formation of subaerial gypsum speleothems (2017)
Attributed to:
Analytical development of the use of the isotopic composition of gypsum hydration water as a paleoclimate tool
funded by
NERC
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