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INFRARED SPECTROSCOPIC STUDY OF SMECTITES OCCURRING IN LOWER SILESIAN BASALT WEATHERING PRODUCTS

In: Geologica Carpathica Clays, vol. 3, no. 1
Krystyna Blaszczak - Wanda S. Sikora - Wieslaw Stuss
Detaily:
Rok, strany: 1994, 27 - 31
O článku:
The smectites from various localities of Lower Silesian basalt weathering products were investigated in the mid-infrared range. They differ mostly in composition of the octahedral sheet. From that point of view aluminium-iron and aluminium-iron-magnesium-smectites can be distinguished. Silicon in tetrahedral sheet is partly substituted by aluminium but the extent of this substitution varies within the samples.
Ako citovať:
ISO 690:
Blaszczak, K., S. Sikora, W., Stuss, W. 1994. INFRARED SPECTROSCOPIC STUDY OF SMECTITES OCCURRING IN LOWER SILESIAN BASALT WEATHERING PRODUCTS. In Geologica Carpathica Clays, vol. 3, no.1, pp. 27-31.

APA:
Blaszczak, K., S. Sikora, W., Stuss, W. (1994). INFRARED SPECTROSCOPIC STUDY OF SMECTITES OCCURRING IN LOWER SILESIAN BASALT WEATHERING PRODUCTS. Geologica Carpathica Clays, 3(1), 27-31.