X-ray diffraction by a randomly interstratified clay mineral; correction
نویسندگان
چکیده
منابع مشابه
Characterization of clay mineral fractions in tuffisitic kimberlite breccias by X-ray diffraction
Kimberlite is described as a diverse and complex hybrid rock in the literature. It is also described as volatile rich, potassic, ultrabasic, igneous rocks that occur as volcanic pipes, dykes and sills1. The minerals present in kimberlites vary widely and can include from trace to predominance any of the following minerals: apatite, calcite, chlorite, diopside (pyroxene), magnetite, monticellite...
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USE of a platy internal standard that will orient to the same degree as clay minerals preserves the relative diffraction intensities between the basal reflections from the platy components, regardless of degree of orientation. The method is illustrated with basic zinc chloride and pyrophyllite as the internal standards for quantitative clay mineral anMysis in the systems kaolinite-liVid illite ...
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ژورنال
عنوان ژورنال: Acta Crystallographica
سال: 1954
ISSN: 0365-110X
DOI: 10.1107/s0365110x54001715