Parnallee). It is of a claret or brownish colour, and possesses the characteristic structure and optical properties of artificial glasses. Some isolated portions of meteorites have also a structure very similar to that of stony lavas, where the shape... Proceedings of the Royal Society of London - Page 337by Royal Society (Great Britain) - 1864Full view - About this book
| 1867 - 524 pages
...Mr. Clifton Sorby, in his microscopical researches into the composition of meteorites, states, that "some isolated portions of meteorites have also a structure very similar to stony lavas " ; and again : " this sometimes gives rise to a structure remarkably like that of consolidated... | |
| 1870 - 442 pages
...mineral was at one time in a state of igneous fusion. The olivin also contains 'gas cavities' like thoee so common in volcanic minerals, thus indicating the...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity... | |
| Charles Knight - 1870 - 446 pages
...met with outside and amongst the crystals, in such a manner as to show that it is the incrystalline residue of the material in which they were formed...glasses. Some isolated portions of meteorites have \lso a structure very similar to that of stony lavas, where the shape and mutual relations of the crystals... | |
| 1865 - 372 pages
...uncrystalline residue of the material in which they were formed. It is of a claret or brownish color, and possesses the characteristic structure and optical...and mutual relations of the crystals to each other proved that they were formed in situ on solidification. A structure is also found so remarkably like... | |
| 1864 - 626 pages
...show that it is the uncrystalline residue of the material in which they were formed ( Mezb'-Madaras, Parnallee). It is of a claret or brownish colour,...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity... | |
| 1864 - 1214 pages
...show that it is the uncrystalline residue of the material in which they were formed (Mezö-Madaras, Parnallee). It is of a claret or brownish colour,...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity... | |
| 1864 - 1632 pages
...The vitreous substance found in the cavities is also met with outside and amongst the crysstals, in such a manner as to show that it is the uncrystalline...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity... | |
| 1866 - 924 pages
...material in which they were formed (Mezo-Madaras, Parnallee). It is of a claret or brownish color, and possesses the characteristic structure and optical...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity... | |
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