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Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite
Atomic-resolution transmission electron microscope evidence mechanism chlorite weathers semi-regular chlorite-vermiculite
2012/3/31
Atomic-resolution transmission electron microscope (TEM) images reveal that IIbb( b5 978 ) Mg,Al,Fe-chlorite from Koongarra, Australia, transforms to vermiculite via a range of intermediate chemical a...
Volumes of K-Na mixing for low albite-microcline crystalline solutions at elevated temperature: A test of regular solution thermodynamic models
K-Na mixing low albite-microcline crystalline solutions elevated temperature test regular solution thermodynamic models
2012/4/1
High-temperature volumes of K-Na mixing have been investigated for a seven-member
low albite-microcline ion-exchange series by conducting X-ray powder diffraction mea-
surements from room temperatur...
Regular Solution Site-Mixing Model for Chlorites
Chlorite Diagenesis Free energy of formation Solid solution Stability
2012/2/6
Activity expressions are presented for a six end-member, regular solution, site-mixing model for chlorites. The end members are ideal 14-侌 chlorites for which experimental stability data are lacking. ...
The “Layer Charge” of Regular Interstratified 2:1 Clay Minerals
Exchange Hydrous Mica Interstratification Mica Mixed-Layers Smectite
2011/11/18
Abstract: Alkylammonium ion exchange on mixed-layer minerals gives detailed information about the variation of cation density in succeeding interlayer spaces. Three mixed layer samples from Japan (sup...
OD-Interpretation of Kaolinite-Type Structures—II: The Regular Polytypes (MDO-Polytypes) and their Derivation
Kaolinite-Type Structures OD-Interpretation MDO-Polytypes
2012/2/14
All MDO-polytypes (i.e. regular polytypes) of trioctahedral, dioctahedral and monoctahedral 1:1 phyllosilicates are derived from their OD-character using the results of our preceding paper. The terms ...