(1915) VI.—The Principle of Saturation. Geological Magazine, S. 6 Vol. 2 (4) 160-164 doi:10.1017/s001675680019185x
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | VI.—The Principle of Saturation | ||
| Journal | Geological Magazine | ||
| Year | 1915 (April) | Series:Volume | 6:2 |
| Page(s) | 160-164 | Issue | 4 |
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s001675680019185x | ||
| Mindat Ref. ID | 263332 | Long-form Identifier | mindat:1:5:263332:3 |
| GUID | f42c25a0-06ba-4297-8e21-a913e72eff3d | ||
| Full Reference | (1915) VI.—The Principle of Saturation. Geological Magazine, S. 6 Vol. 2 (4) 160-164 doi:10.1017/s001675680019185x | ||
| Plain Text | (1915) VI.—The Principle of Saturation. Geological Magazine, S. 6 Vol. 2 (4) 160-164 doi:10.1017/s001675680019185x | ||
| In | (1915, April) Geological Magazine S. 6 Vol. 2 (4) Cambridge University Press (CUP) | ||
| Abstract/Notes | In Professor Shand's reply to my criticism of his original paper on the application of the principle of saturation with respect to silica in the classification of igneous rocks, some points arise which make it clear that he has misunderstood me in several particulars. In the beginning of my paper, it was explicitly stated that what was to be considered was (1) whether the principle, as enunciated by Professor Shand, could be extended to minerals other than the silica ones (quartz, tridymite, etc.), the felspars and the felspathoids, and (2) whether the criterion whereby the rock minerals were divided into the two groups of saturated and unsaturated was sufficiently exact. The criterion used was that of “the observed facts of distribution”, and any mineral which was found coexisting with quartz or some other form of silica in igneous rocks was said to be saturated, while those which did not occur along with quartz were said to be unsaturated. Correspondingly, rocks which consisted entirely of minerals of the former type were classed as saturated, those consisting of mixtures of the two types as part-saturated, and those consisting solely of the second type as unsaturated. I endeavoured to show that the rock-forming minerals cannot be satisfactorily divided into two classes in this empirical fashion, without any consideration of the cooling-histories of the individual rocks in which the minerals may be found. | ||
References Listed
These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
| Tyrrell (1912) Trans. Glas. Geol. Soc. xiv, 238 | |
| Rosenbusch (1905) Mikroskopische Physiographie ii, 151 | |
| (1883) Compt. Rend. xcvi, 1303 | |
| Gorgeu (1883) Ann. chim. phys. iv, 515 | |
| Not Yet Imported: American Journal of Science - journal-article : 10.2475/ajs.s4-4.20.105 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 4057 | |
| (1895) Zeit. Kryst. Min. xxv, 375 | |
| (1905) Mikroskopische Physiographie ii, 25 | |
| (1911) Journ. Ind. Eng. Chem. iii, 10 | |
| Harker (1907) Science Progress ii, 242 | |
| (1914) Amer. Journ. Sci. xxxvii, 487 | |
| (1914) Journ. Geol. xxii, 16 | |
| Not Yet Imported: American Journal of Science - journal-article : 10.2475/ajs.s4-31.181.25 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 4057 | |
| (1914) Zeit. für Anorg. Chem. lxxxvii, 283 | |
| Rosenbusch (1910) Elemente der Gesteinlehre , 458 | |
| (1913) Geol. Mag., Dec. V X, 508 | |
| (1909) Geol. Mag., Dec. V VI, 299 | |
| (1904) Die Silikatschmelelösungen ii, 66 | |
| (1886) Bull. Soc. Min. Franç. ix, 40 | |
| Shand (1909) Trans. Edin. Geol. Soc. ix, 205 | |
| (1847) Comptes Rendus xxiv, 784 | |
| Vogt () loc. cit. ii, 112 |
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