Essentials for the Microscopical Determination of Rock Forming Minerals And Rock
Essentials for the Microscopical Determination of Rock Forming Minerals And Rock
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Zoisite has parallel extinction, different color, and smaller optic angle. Clinozoisite has different cleavage (001:100 = 6437'), and usually abnormal interference colors.
Staurolite occurs in crystalline schists as a contact or dynamo-metamorphic mineral. In- clusions symmetrically arranged or in subparallel bands are common. The yellow, red, or brown color, the pleochroism, c = red-brown, a and b = yellow, the parallel extinction, the large optic angle, 2V = 89, giving a straight bar in secti...ons at right angles to an optic axis, separate it from other minerals. Andalusite is negative and has different pleochroism, g e d r i t c has smaller optic axial angle (2V = 57-79) and amphibole cleavage, anthophyllite has amphibole cleavage and is rarely pleochroic in thin sections, vesuvianite has a pale yellow color, is negative, and has lower birefringence.
Clinochlore, one of the chlorites, occurs in leaves, scales, plates, or leafy aggregates as a min- eral of schists and serpentines, and as a secondary mineral in igneous rocks from the alteration of ferromagnesian silicates.
What to read after Essentials for the Microscopical Determination of Rock Forming Minerals And Rock?
You can find similar books in the "Read Also" column, or choose other free books by Albert Johannsen to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Zoisite has parallel extinction, different color, and smaller optic angle. Clinozoisite has different cleavage (001:100 = 6437'), and usually abnormal interference colors.
Staurolite occurs in crystalline schists as a contact or dynamo-metamorphic mineral. In- clusions symmetrically arranged or in subparallel bands are common. The yellow, red, or brown color, the pleochroism, c = red-brown, a and b = yellow, the parallel extinction, the large optic angle, 2V = 89, giving a straight bar in secti...ons at right angles to an optic axis, separate it from other minerals. Andalusite is negative and has different pleochroism, g e d r i t c has smaller optic axial angle (2V = 57-79) and amphibole cleavage, anthophyllite has amphibole cleavage and is rarely pleochroic in thin sections, vesuvianite has a pale yellow color, is negative, and has lower birefringence.
Clinochlore, one of the chlorites, occurs in leaves, scales, plates, or leafy aggregates as a min- eral of schists and serpentines, and as a secondary mineral in igneous rocks from the alteration of ferromagnesian silicates.
What to read after Essentials for the Microscopical Determination of Rock Forming Minerals And Rock?
You can find similar books in the "Read Also" column, or choose other free books by Albert Johannsen to read onlineMoreLess
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