Method and system for determining protrusion grade of transparent minerals in rock, and application of system
A determination method and technology of minerals, applied in the field of determination of grades and grades, can solve problems such as identification errors of mineral components, and achieve the effect of intuitive determination and simple operation methods
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Embodiment 1
[0048] A method for determining the grade of transparent mineral protrusions, especially a method for quickly and accurately determining the grade of mineral protrusions under an orthogonal polarizing microscope.
[0049] It includes the following steps:
[0050]Find the minerals to be tested under an orthogonal polarizing microscope by grinding medium-fine-grained igneous rock slices with a thickness of 0.03 mm (mineral particle diameter > 0.5 mm);
[0051] Minerals to be tested should meet the following characteristics:
[0052] 1. The edge of the mineral part to be tested is in contact with Canada gum;
[0053] 2. The edge of the part of the mineral to be tested is in contact with the known mineral;
[0054] In this embodiment, part of the edge of the mineral to be tested is in contact with the gum, and part of the edge is in contact with the known mineral quartz. By observing the protruding height of the mineral to be tested relative to the gum and quartz, the protrudin...
Embodiment 2
[0060] A method for determining the grade of transparent mineral protrusions, especially a method for quickly and accurately determining the grade of mineral protrusions under an orthogonal polarizing microscope.
[0061] It includes the following steps:
[0062] Find the minerals to be tested under an orthogonal polarizing microscope by grinding medium-fine-grained igneous rock slices with a thickness of 0.03 mm (mineral particle diameter > 0.5 mm);
[0063] Minerals to be tested should meet the following characteristics:
[0064] 1. The edge of the mineral part to be tested is in contact with Canada gum;
[0065] 2. The edge of the part of the mineral to be tested is in contact with the known mineral;
[0066] In this embodiment, two adjacent mineral particles are considered to belong to the same mineral particle from the crystal shape and interference color, but they can be clearly distinguished through the observation of the protrusions.
[0067] Observation under 10x o...
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