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Kaolinization and other changes in West of England rocks

Published online by Cambridge University Press:  14 March 2018

Extract

The behaviour of a mass of molten but cooling igneous rock under moderate pressure may be compared to that of liquid cupelled silver, which at a certain temperature can no longer retain the oxygen, many times its volume, that it has occluded. Thus, during the submarine eruption off the island of Pantelleria in 1891, blocks of lava that swam for a while on the surface of the sea exploded with violence. Chilling by contact with sea-water had occasioned exactly what Lowthian Bell observed to happen on the sudden cooling of masses of slag by contact with water. There was a discharge within the set outer envelope, at something near a red heat, of previously dissolved water and gases, converting the floating ejectamenta into a species of bombs.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1908

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References

Page 128 note 1 Bell, L., Journ. Iron and Steel Inst., 1881, pp. 534 Google Scholar and 540.

Page 128 note 2 Sorby, H. C., Quart. Journ. Geol. Soc., 1858, vol. xiv, p. 489.Google Scholar

Page 129 note 1 Dutton, C. E., Amer. Journ. Sci., 1883, vol. xxv, pp. 220221 Google Scholar.

Page 129 note 2 Fisher, O., ‘Physics of tile Earth's Crust.’ 2nd edit., 1889, pp. 47 Google Scholar and 51.

Page 129 note 3 Flett, J. S., Mem. Geol. Surv., Land's End District, 1907, p. 50 Google Scholar.

Page 129 note 4 Allport, S., Quart. Journ. Geol. Soc., 1876, vol. xxxii, p. 41 Google Scholar

Page 129 note 5 Smith, Michie, Proc. R. Soc. Edinburgh, 1889-90, vol. xvii, p. 65 Google Scholar.

Page 130 note 1 A blast-furnace slag from Trignae, Allier, France, in the British Museum (Natural History) collection yields hydrogen sulphide as readily as fetid barytes when scratched.

Page 130 note 2 L. Bell, loc. cit., p. 541.

Page 130 note 3 Angelot, J. F., Bull. Soc. Géol. France, 1842, sér. 1, vol. xiii, pp. 188189.Google Scholar

Page 130 note 4 Kemp, J. F., in ‘The Genesis of Ore-Deposits,’ published by the Amer. Inst, Mining Eng., 2nd edit., 1902, pp. 687688 Google Scholar.

Page 130 note 5 Chamberlin, T. C. and Salisbury, R. D., ‘Geology,’ 1904, vol. i, p. 607.Google Scholar

Page 130 note 6 Johnston-Lavis, H. J., Quart. Journ. Geol. Soc., 1885, vol. xli, Proc., p. 104 Google Scholar

Page 130 note 7 Sorby, H. C., Quart. Journ. Geol. Soc., 1858, vol. xiv, p. 475 Google Scholar.

Page 130 note 8 Allport, S., Quart. Journ. Geol. Soc., 1876, vol. xxxii, p. 408.Google Scholar

Page 131 note 1 Seemingly not detectible in the first microscopic preparation. (See Bonney, T. G., Trans. R. Geol. Soc. Cornwall, 1883, vol. x, pp. 180186 Google Scholar.)

Page 131 note 2 Judd, J. W., Quart. Journ. Geol. Soc., 1889, vol. xlv, p. 181 Google Scholar

Page 131 note 3 Arrhenius, S., in ‘The Genesis of Ore-Deposits,’ sup. cit., p. 644.Google Scholar

Page 132 note 1 J. S. Flett, loc. cit.

Page 133 note 1 Collins, J. H., ‘The Hensbarrow Granite District.’ 1878, p. 9 Google Scholar.

Page 133 note 2 Rosenbusch, H., ‘Microscopic Physiography of the Rock-making Minerals,’ transl. J. P. Iddings, 4th edit, 1898, p. 108 Google Scholar.

Page 133 note 3 Sedgwick, A., Trans. Cambridge Phil. Soc., 1821, vol. i, pp. 105106 Google Scholar.

Page 134 note 1 Scharizer, R., Zeits. Kryst. Min., 1887, vol. xv, p. 343 Google Scholar.

Page 134 note 2 R. Scharizer, loc. cit., pp. 348-349.

Page 134 note 3 Teall, J. J. H., ‘British Petrography.’ 1888, p. 316 Google Scholar.

Page 134 note 4 See Bonney, T. G., ‘On the microscopic structure of trowlesworthite.’ Trans. R. Geol. Soc. Cornwall, 1883, vol. x, pp. 180186 Google Scholar.

Page 135 note 1 Allport, S., Quart. Journ. Geol. Soc., 1876, vol. xxxii, p. 416.Google Scholar

Page 136 note 1 Collins, J. H., ‘The Hensbarrow Granite District.’ 1878, p. 31.Google Scholar

Page 136 note 2 Lindgren, W., in ‘The Genesis of Ore-Deposits,’ op. cit., 1902, 2nd edit., p. 530.Google Scholar

Page 136 note 3 J. H. L. Vogt, ibid, pp. 661-668.

Page 137 note 1 Collins, J. H., Min. Mag., 1887, vol. vii, pp. 212214 Google Scholar.

Page 137 note 2 Penrose, R. A. F., 16th Ann. Rap. U. S. Geol. Surv., Pt. 2, 1895, p. 128 Google Scholar et pass.

Page 137 note 3 See SirLyell, Charles, ‘Principles of Geology,’ 1867, vol. i, p. 413 Google Scholar; Scrope, G. P., ‘Volcanos,’ 2nd edit., 1872, p. 152 Google Scholar.

Page 137 note 4 Le Neve Foster, C., Trans. R. Geol. Soc. Cornwall, 1883, vol. x, p. 176 Google Scholar.

Page 137 note 5 Penrose, loc. cit.

Page 138 note 1 Rösler, H., Neues Jahrb. Min., 1902, Beilage-Band xv, p. 276 Google Scholar.

Page 138 note 2 Schmidt, C. W., Zeits. Deutsch. geol. Ges., 1885, vol. xxxvii, p. 739 Google Scholar.

Page 138 note 3 de Lapparent, A., Bull. Soc. Géol. France. 1889, sér. 8, vol. xvii, pp. 286287 Google Scholar. Cf. Judd, J. W., Quart. Journ. Geol. Soc., 1890, vol. xlvi, pp. 368369 Google Scholar.

Page 138 note 4 Zezi, P., in ‘The South Italian Volcanoes,’ ed. by Johnston-Lavis, H. J., Naples, 1891, p. 88 Google Scholar.

Page 138 note 5 On Cornish calcareous rocks, see De la Beche, H. T., ‘Report on the Geology of Cornwall, &c.,’ 1839, pp. 7989 Google Scholar, etloass.

Page 138 note 6 Sorby, H. C., Quart. Journ. Geol. Soc., 1858, vol. xiv, pp. 471 Google Scholar and 4

Page 138 note 7 Phillips, J. A., Phil. Mag., 1871, ser. 4, vol. xlii, pp. 408413 Google Scholar.

Page 139 note 1 H. T. De la Beche, loc. cit., p. 88.

Page 139 note 2 Phillips, J. A., Quart. Journ. Geol. Soc., 1878, vol. xxxiv, pp. 477, 482-484.Google Scholar

Page 139 note 3 Daubrée, A., Quart. Journ. Geol. Soc., 1878, vol. xxxiv, pp. 7374.CrossRefGoogle Scholar

Page 141 note 1 A. Daubréo, loc. cit., p. 74.

Page 142 note 1 Bonney, T. G., Min. Mag., 1877, vol. i, pp. 216217.Google Scholar

Page 142 note 2 Scrivenor, J. B., Quart. Journ. Geol. Soc., 1903, vol. lix, p. 151 Google Scholar, and Mem. Geol. Surv. Eng. & Wales, Geol. of Newquay, 1906, p. 44.

Page 142 note 3 Brögger, W. C. (Zeits. Kryst. Min., 1890, vol. xvi, p. 655)Google Scholar describes a tourmaline occurring in analcime and calcite at Langesundfjord, and showing, from within outwards, a blue nucleus, a deeper blue intermediate zone, and a brown marginal zone.

Page 143 note 1 Bonney, T. G., Min. Mag., 1877, vol. i, pp. 216217.Google Scholar

Page 143 note 2 Le Neve Foster, C., Trans. R. Geol. Soc. Cornwall, 1887, vol. x, pp. 8 and 9Google Scholar.

Page 145 note 1 R. A. F. Penrose, loc. cit.

Page 145 note 2 Sorby, H. C., Quart. Journ. Geol. Soc., 1858, vol. xiv, p. 494.Google Scholar

Page 145 note 3 J. F. Kemp, loc. cit., pp. 696-702 and 709.