The significance of hydrogen and oxygen stable isotopic fractionations between carnallite and brine at low temperature: Experimental and empirical results-Reference-Cited by-同舟云学术

The significance of hydrogen and oxygen stable isotopic fractionations between carnallite and brine at low temperature: Experimental and empirical results

Published:1996-07 Issue:14 Volume:60 Page:2721-2726
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Koehler Geoff,Kyser T.K.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference24 articles.

1. RbSr and KCa isotope systematics in minerals from potassium horizons in the Prairie Evaporite Formation, Saskatchewan, Canada;Baadsgaard;Chem. Geol.,1987

2. Fluid inclusion evidence for the deposition and diagenesis of the Patience Lake Member of the Prairie Evaporite Formation;Chipley;Sediment. Geol.,1989

3. Preservation of ancient basinal fluids in halite fluid inclusions;Chipley,1992

4. Stable isotope fractionation factors of water in hydrated saline mineral-brine systems;Horita;Earth Planet. Sci. Lett.,1989

5. Analytical aspects of stable isotopes in brines;Horita;Chem. Geol.,1989

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1. Stable Isotopic Composition of Hydration Water in Carnallite of Late Cretaceous Potash Deposits on Khorat Plateau;Acta Geologica Sinica - English Edition;2014-12

2. Geochemistry of Evaporites and Evolution of Seawater;Treatise on Geochemistry;2014

3. Method for Simultaneous Oxygen and Hydrogen Isotope Analysis of Water of Crystallization in Hydrated Minerals;Analytical Chemistry;2008-08-20

4. Equilibrium Oxygen, Hydrogen and Carbon Isotope Fractionation Factors Applicable to Geologic Systems;Reviews in Mineralogy and Geochemistry;2001-01-01