Article navigation
JOURNAL ARTICLE
Thermodynamic properties of some 2:1 layer clay minerals from solution-equilibration data
Stephen U. Aja
Stephen U. Aja
City University of New York, Brooklyn College, Department of Geology, Brooklyn, NY, United States
Search for other works by this author on:
European Journal of Mineralogy (1995) 7 (2): 325-333.
Published:
April 01, 1995
Search
Search
Sign in
Don't already have an account? Register
You could not be signed in. Please check your email address / username and password and try again.
Index Terms/Descriptors
Citing articles via
Related Articles
C – Goldschmidt Abstracts 2013
Mineralogical Magazine
F – Goldschmidt Abstracts 2013
Mineralogical Magazine
M – Goldschmidt Abstracts 2013
Mineralogical Magazine
T – Goldschmidt Abstracts 2013
Mineralogical Magazine
D – Goldschmidt Abstracts 2013
Mineralogical Magazine
I – Goldschmidt Abstracts 2013
Mineralogical Magazine
Related Book Content
Nanoscale Imaging of Organic Matter and Wettability of Oil-Window Shales
Imaging Unconventional Reservoir Pore Systems
Mineralogy and petrology of the Paleocene Clayton and Porters Creek Formations, Missouri, USA: Influence of Cretaceous-Paleogene impact debris and diagenesis
Paying Attention to Mudrocks: Priceless!
High-pressure mineralogy of diamond genesis
Advances in High-Pressure Mineralogy
Stable isotopic evidence for a pre–late Miocene elevation gradient in the Great Plains–Rocky Mountain region, USA
Tectonics, Climate, and Landscape Evolution
Chloritic minerals from prehnite-pumpellyite facies rocks of the Winterville Formation, Aroostook County, Maine
Low-Grade Metamorphism of Mafic Rocks
The Cretaceous/Tertiary boundary interval, Raton Basin, Colorado and New Mexico, and its content of shock-metamorphosed minerals; Evidence relevant to the K/T boundary impact-extinction theory
The Cretaceous/Tertiary boundary interval, Raton Basin, Colorado and New Mexico, and its content of shock-metamorphosed minerals; Evidence relevant to the K/T boundary impact-extinction theory