A Summary of Progress in Petrography. in 1887-1896 |
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Page 11
... nature is discoverable only by optical methods . In order to show their relations to the Willemite 8 Zeits . f . Kryst . , XVIII . , 1890 , p . 361 . USE ce al ly te on er- rst by us- 1891. ] 141 Mineralogy and Petrography .
... nature is discoverable only by optical methods . In order to show their relations to the Willemite 8 Zeits . f . Kryst . , XVIII . , 1890 , p . 361 . USE ce al ly te on er- rst by us- 1891. ] 141 Mineralogy and Petrography .
Page 14
... , 1890 , p . 94 . 16 Ib . , p . 215 . 17 Zeits . f . Kryst . , XVIII . , 1890 , p . 114 . 18 Miner . u . Petrog . Mitth . , XI . , 1890 , p . 349 . graphic directions , and different along unequivalent directions . Further MAKER.
... , 1890 , p . 94 . 16 Ib . , p . 215 . 17 Zeits . f . Kryst . , XVIII . , 1890 , p . 114 . 18 Miner . u . Petrog . Mitth . , XI . , 1890 , p . 349 . graphic directions , and different along unequivalent directions . Further MAKER.
Page 14
... . , etc. , B. B. , VII . , p . 152 . 22 Neues Jahrb . f . Min . , etc. , B. B. , VII . , p . 175 . 23 Zeits . f . Kryst . , XVIII . , 1890 , p . 44 . In a -n ex ns or . for of Iso is late 1891. ] 145 Mineralogy and Petrography .
... . , etc. , B. B. , VII . , p . 152 . 22 Neues Jahrb . f . Min . , etc. , B. B. , VII . , p . 175 . 23 Zeits . f . Kryst . , XVIII . , 1890 , p . 44 . In a -n ex ns or . for of Iso is late 1891. ] 145 Mineralogy and Petrography .
Page 14
... Kryst . , XVIII . , 1890 , p . 209 . WTI Fe as with seri the they ana cal nose som a m auth Upo ultra by the of lapis subs char a lit an Chil are desc a yel posit The the was r of th Helvite may be nite , Capa in ra M • Ze scrip- more ...
... Kryst . , XVIII . , 1890 , p . 209 . WTI Fe as with seri the they ana cal nose som a m auth Upo ultra by the of lapis subs char a lit an Chil are desc a yel posit The the was r of th Helvite may be nite , Capa in ra M • Ze scrip- more ...
Page 14
... , and specific gravity 2.17 . Miner . u . Petrog . Mitth . , XI . , 1890 , p . 214 . 8 • Zeits . f . Kryst . , 1882 , VI . , ) p . 627 . H 9 = They remain unchanged in the air , and [ April , 369 1891. ] Mineralogy and Petrography .
... , and specific gravity 2.17 . Miner . u . Petrog . Mitth . , XI . , 1890 , p . 214 . 8 • Zeits . f . Kryst . , 1882 , VI . , ) p . 627 . H 9 = They remain unchanged in the air , and [ April , 369 1891. ] Mineralogy and Petrography .
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Common terms and phrases
acid Al,O alteration Amer AMERICAN NATURALIST analysis andalusite angle aragonite augite axial ratio basalts beryl biotite brucite Bull calcite calcium chlorite cleavage Colby University color colorless composition constituents containing cordierite corresponding crystalline crystals density described diabase double refraction dyke eruptive rocks Fe,O Fe₂O feldspar FeO MgO CaO FeO MnO forms formula Franc gabbro-diorites gabbros garnet Genth gneisses granite granulites ground-mass H₂O habit hexagonal hornblende humite hypersthene imbedded inclusions Jour Kryst leucite masses melanophlogite metacinnabarite mica mineral MINERALOGY AND PETROGRAPHY.¹ Mitth molecules muscovite Neues Jahrb nosean occur olivine optical original orthoclase ottrelite parallel Penfield Petrog PETROGRAPHY.¹ Petrographical phenacite plagioclase plane plates polymorphism prismatic produced pseudomorphs pyroxene quartz regarded rock individual Rosenbusch schistose schists serpentine silica sodium soluble specific gravity specimens spinel structure substance sulphur symmetry tabular temperature tonalite tourmaline twinned varieties W. S. Bayley Waterville yielded Zeits zircon zone
Popular passages
Page 19 - The plane of the optical axes is perpendicular to the plane of symmetry, and makes with c an angle of °7 in acute /9. A = b. 2H na = 104° 27'.
Page 14 - The larger part of the dust is thought to be a sediment from the air, and to have been obtained by it from a region of crystalline schists. The chondri, on the other hand, are thought to be of cosmic origin, since they are similar to the chondri obtained in deep-sea soundings. If the amount of the dust collected from the snow in Greenland represents the fall of one year, the total amount falling upon the entire surface of the earth in this time is 125 million kilograms, equivalent to a cube of thirty-one...
Page 14 - Wiilfing 21 for investigation, by whom it has been found to consist in greater part of feldspar, quartz, mica, and hornblende. There are present in it also garnet, zircon, magnetite, augite, and sillimanite, and with them is mixed a nitrogenous organic substance. The most interesting constituents of the dust...