In: Geologica Carpathica Clays, vol. 5, no. 2
Andrzej Wiewiora - Andrzej Wilamowski
Detaily:
Rok, strany: 1996, 79 - 87
O článku:
On the basis of the outlines of the crystallochemical classification of chlorites (Wiewióra & Weiss 1990), the authors postulate regression equations for the b parameter, derived from the published structural and chemical data of chlorites:
— trioctahedral chlorites
b=9.225+0.0270AlIV-0.0386AlVI+0.0376Fe2+ -0.0376Cr3+ +0.0665Mn2+
— di-tri- and di-dioctahedral chlorites
b=8.860+0.112AlIV+0.0524Mg2++0.0752Fe2++O.0600Fe3+ -0.0523Li+
These equations, together with the similar regression equation for d(001) derived by Raussel-Colom, Wiewióra & Matesanz (1991), were used to prepare 2D and 3D diagrams. They may be used for estimation of the chemical composition of any chlorite from the XRD analysis.
— trioctahedral chlorites
b=9.225+0.0270AlIV-0.0386AlVI+0.0376Fe2+ -0.0376Cr3+ +0.0665Mn2+
— di-tri- and di-dioctahedral chlorites
b=8.860+0.112AlIV+0.0524Mg2++0.0752Fe2++O.0600Fe3+ -0.0523Li+
These equations, together with the similar regression equation for d(001) derived by Raussel-Colom, Wiewióra & Matesanz (1991), were used to prepare 2D and 3D diagrams. They may be used for estimation of the chemical composition of any chlorite from the XRD analysis.
Ako citovať:
ISO 690:
Wiewiora, A., Wilamowski, A. 1996. THE RELATIONSIP BETWEEN COMPOSITION AND b FOR CHLORITE. In Geologica Carpathica Clays, vol. 5, no.2, pp. 79-87.
APA:
Wiewiora, A., Wilamowski, A. (1996). THE RELATIONSIP BETWEEN COMPOSITION AND b FOR CHLORITE. Geologica Carpathica Clays, 5(2), 79-87.