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CLAY MINERALS
Rivista
Codice:
E037858
ISSN:
0009-8558
Dati Generali
Dati Generali
Pubblicazioni (18)
Pulisci
Ordina Pubblicazioni:
ascendente
decrescente
A method for determining the CEC and chemical composition of clays via XRF.
Articolo
Alteration of clay minerals in a sedimentary caprock and its use in geothermal prospecting: an example from Mt. Amiata
Articolo
An approach to the chem¬istry of pyroxenes formed during the firing of Ca-rich silicate ceramics
Articolo
Clay mineral reactions in an active geothermal area (Mt. Amiata, southern Tuscany, Italy).
Articolo
Clayey materials from the Sierra de la Demanda Range (Spain): their potential as raw materials for building ceramic industry
Articolo
Corrensite and chlorite-rich Chl-S mixed layers in sandstones from the 'Macigno' Formation (northwestern Tuscany, Italy)
Articolo
Fine-grained weathering products in waste disposal from two sulphide mines of the Northern Apennines, Italy
Articolo
Geochemical and mineralogical approaches to assessing provenance and deposition of shales: a case study
Articolo
Geochemical and mineralogical approaches to assessing provenance and deposition of shales: a case study
Articolo
Grain size distribution of Italian raw materials for structural clay products: a reappraisal of the Winkler diagram
Articolo
In situ transformation of amorphous gels into spherical aggregates of kaolinite: A HRTEM study
Articolo
Interaction between glycine and Na-, Ca-, and Cu-rich smectites
Articolo
K-rich rectorite from kaolinized micaschist of Sesia-Lanzo Zone (Italy)
Articolo
Newly formed phyllosilicates in rock matrices and fractures from CRP-3 core (Antarctica): An electron microscopy study
Articolo
Newly-formed phyllosilicates in sediments and basement rocks from CRP-3 core (Antarctica): An electron microscopy study.
Articolo
Smectite formation in rhyolitic obsidian as inferred by microscopic (SEM-TEM-AEM) investigation.
Articolo
The influence of layer-charge on Zn2+ and Pb2+ sorption by smectites
Articolo
Variations in the chemical composition of illite from five geothermal fields: a possibile geothermometer.
Articolo
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