KAOLIN-GROUP MINERALS FROM THE HYDROTHERMAL MERCURY DEPOSIT AT RAKOS (CENTRAL SLOVAKIA)

Rok, strany: 1996, 73 - 78

A soft white day occurring in diverse types of are mineralization as lenses, cavity and veinlet fillings in the Rakos hydrothermal mercury deposit is shown by X-ray powder diffraction, SEM, thermal and chemical analyses to be essentially well ordered 1 Tc kaolinite, sub-ordinate dickite or mixture of both. These kaolin-group minerals crystallized from solutions and can be regarded as genetically associated with the youngest cinnabar mineralization.

ISO 690:

Samajova, E., Fejdi, P. 1996. KAOLIN-GROUP MINERALS FROM THE HYDROTHERMAL MERCURY DEPOSIT AT RAKOS (CENTRAL SLOVAKIA). In Geologica Carpathica Clays, vol. 5, no.1, pp. 73-78.

APA:

Samajova, E., Fejdi, P. (1996). KAOLIN-GROUP MINERALS FROM THE HYDROTHERMAL MERCURY DEPOSIT AT RAKOS (CENTRAL SLOVAKIA). Geologica Carpathica Clays, 5(1), 73-78.