Distinguished five groups of samples, characterized by the prevailing, each time, of Ba-phillipsite or wellsite or harmotome compositions. The diffractometric behaviour shows good correlations with the BaO content of natural samples. The genetic features of the sedimentary deposits of Ba-zeolitic materials and the coexistence of different compositions into the same deposit, were discussed
Distinzione di termini Ba-zeolitici attraverso il loro comportamento diffrattometrico e termico dopo scambio con K e Ba
Tateo;
1990
Abstract
Distinguished five groups of samples, characterized by the prevailing, each time, of Ba-phillipsite or wellsite or harmotome compositions. The diffractometric behaviour shows good correlations with the BaO content of natural samples. The genetic features of the sedimentary deposits of Ba-zeolitic materials and the coexistence of different compositions into the same deposit, were discussedFile in questo prodotto:
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