No CrossRef data available.
Article contents
III.—A Discussion on the Use of the Terms Rock-weathering, Serpentinization, and Hydrometamorphism
Published online by Cambridge University Press: 01 May 2009
Extract
In the abstract of a paper by Mr. Thomas H. Holland, read before the British Association, Section C (Geology), Bristol, 1898, printed in the January number of this Magazine, on “The Comparative Actions of Subaërial and Submarine Agents in Rock Decomposition,” the author brings up again a question which the present writer has often had occasion to face, and has vainly tried to solve in a manner entirely satisfactory even to himself.
- Type
- Original Articles
- Information
- Copyright
- Copyright © Cambridge University Press 1899
References
page 354 note 1 Geol. Mag., January, 1899, pp. 30–1.
page 355 note 1 17th Ann. Rep. U.S.G.S., 1895–6, pt. ii, pp. 90–6.
page 355 note 2 “Rocks and Rock-weathering,” pp. 188, 234, etc.
page 356 note 1 In part due to C 0, though the amount of this constituent cannot be over 3 or 4 per cent.
page 356 note 2 J. Smith, “Crystals from Decomposed Trap”: Geol. Mag., Dec. IV, Vol. VI (1899), p. 93.
page 357 note 1 “Chemical and Physical Geology,” Paul&Drummond's English translation, 1854, vol. iii, p. 86.
page 357 note 2 “Über den Serpentin, etc.”: Abhandl. der K. Akademie der Wiss. zu Berlin, ii (1869), p. 42.
page 357 note 3 “Allegemeine u. Chemische Geologie,” 1893.
page 357 note 4 “British Petrography,” p. 85.