Rock Forming Minerals
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In our eReader you can find the full English version of the book. Read Rock Forming Minerals Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Rock Forming Minerals
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- P (111) . P oo (101) and OP (001). Twin crystals are common, and the twinning is upon a plane parallel to the orthopinacoid oo P oo(100). Sections parallel to this face do not therefore show the twinning, but in those parallel to the clinopinacoid (010) and the prism (110) it is distinctly seen. A zoned structure, due to the successive growth of layers, which differ more or less in composition through isomorphous substitution, is frequently met with in augite crystals. The cleavage is paralle...l to oo P (110) and to oo P oo (100) ; but the former, although at times it is clearly visible in basal sections, or in sections transverse to the prism, is at others very obscure or quite imperceptible. When this cleavage appears, it can easily be distinguished from that of hornblende by the planes, which are often interrupted, intersecting nearly at right angles (87 6') ; while in hornblende the angle is about thirty-three degrees wider, and the difference can, there- fore, be detected at a glance.
What to read after Rock Forming Minerals?
You can find similar books in the "Read Also" column, or choose other free books by Frank Rutley to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
- P (111) . P oo (101) and OP (001). Twin crystals are common, and the twinning is upon a plane parallel to the orthopinacoid oo P oo(100). Sections parallel to this face do not therefore show the twinning, but in those parallel to the clinopinacoid (010) and the prism (110) it is distinctly seen. A zoned structure, due to the successive growth of layers, which differ more or less in composition through isomorphous substitution, is frequently met with in augite crystals. The cleavage is paralle...l to oo P (110) and to oo P oo (100) ; but the former, although at times it is clearly visible in basal sections, or in sections transverse to the prism, is at others very obscure or quite imperceptible. When this cleavage appears, it can easily be distinguished from that of hornblende by the planes, which are often interrupted, intersecting nearly at right angles (87 6') ; while in hornblende the angle is about thirty-three degrees wider, and the difference can, there- fore, be detected at a glance.
What to read after Rock Forming Minerals?
You can find similar books in the "Read Also" column, or choose other free books by Frank Rutley to read onlineMoreLess
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