Dissection and correlation of red-colored strata on the basis of X-ray diffractometric analysis of clay fraction minerals
Authors:
About authors
- Postgraduate student G.V. Plekhanov Saint Petersburg Mining Institute
Abstract
Analysis of red terrigenous rocks with application of the X-ray diffraction method was carried out as part of the research on the example of Upper-Sorbian sediments of the Southeastern part of the White Sea region. The first results of the experimental research are considered and the possibility was shown to differentiate and correlate red beds basing on x-ray characteristics of fine fraction of the rocks.
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