SY/T 6210-1996 X-ray Diffraction Quantitative Analysis Method of Total Clay Minerals and Common Non-clay Minerals in Sedimentary Rocks (English Version)
This standard specifies sample preparation, test conditions, quantitative analysis methods and quality requirements for analysis results using X-ray diffraction technology to determine the total amount of clay minerals and the content of common non-clay minerals in sedimentary rocks. This standard applies to the total amount of clay minerals in sedimentary rocks and quartz, calcite, dolomite, ankerite, siderite, anhydrite, gypsum, anhydrous mirabilite, barite, pyrite, halite, plagioclase, Qualitative and quantitative analysis of common non-clay minerals such as potassium feldspar, glauberite, turbidite, and analcime.
SY/T 6210-1996 history
2018SY/T 5163-2018 X-ray diffraction analysis method of clay minerals and common non-clay minerals in sedimentary rocks
2010SY/T 5163-2010 Analysis method for clay minerals and ordinary non-clay minerals in sedimentary rocks by the X-ray diffraction
1996SY/T 6210-1996 X-ray Diffraction Quantitative Analysis Method of Total Clay Minerals and Common Non-clay Minerals in Sedimentary Rocks
SY/T 6210-1996 X-ray Diffraction Quantitative Analysis Method of Total Clay Minerals and Common Non-clay Minerals in Sedimentary Rocks was changed to SY/T 5163-2010 Analysis method for clay minerals and ordinary non-clay minerals in sedimentary rocks by the X-ray diffraction.