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I.—The Carrara Marbles. A Chapter in the History of Continental Geology

Published online by Cambridge University Press:  01 May 2009

G. A. Lebour
Affiliation:
London and Belgium, Lecturer in Geological Surveying in the University of Durham College of Physical Science, Newcastle-on-Tyne.

Extract

The celebrated statuary marbles of Carrara, which have of late I years been universally described as of Jurassic age, have quite recently been shown conclusively to belong to the Carboniferous series, and the steps which have led to the discovery form an instructive illustration of the difficulties which beset Alpine Geology. No one has a better right to relate the history of the classification of the rocks of the Apuan Alps than M. Coquand, and this he is now doing in a series of papers published in the Bulletin of the Geological Society of France. From the first of these we arrive at the following résumé of the various opinions which have been held-from time to time regarding the age of the statuary marbles.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1876

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References

page 289 note 1 Coquand, H., “Histoire des Terrains stratifiés de l'ltalie centrale se référant aux périodes primaire, paléozoïque, triasique, rhétienne et jurassique,” Bull. Soc. Géologique de France, 3e sér. tom. iii. p. 27 (1875).Google Scholar

page 289 note 2 In a paper published in the “Nuovo Giornale dei Litterati,” t. xxvii. (1833 ?).

page 289 note 3 “Sur les terrains stratifiés de la Toscane,” Bull. Soc. Géol. France, 2e sér. t. ii. p. 155 (1844–45).Google Scholar

page 289 note 4 Atti Scienz. Ital. p. 568 (1844).

page 290 note 1 “Saggio comparative dei terreni che componzono il suolo d'ltalia,” Ann. Univ. Tosc. Sci. Cosm. Pisa, t. i. p. 205 (1846).Google Scholar

page 290 note 2 “Sur un gisement de gypse au promontoire Argentaire,” Bull. Soc. Géol. France, 2e sér. t. iii. p. 302 (1845–46).Google Scholar

page 290 note 3 “Sur le calcaire rouge ammonitifère de l'ltalie,” Bull. Soc. Géol. France, 2e sér. t. iv. p. 1062 (1846–47).Google Scholar

page 290 note 4 “Sulla costituzione geologica dei Monti Pisani,” 1846.

page 290 note 5 “Description des roches ignées et sédimentaires de la Toscane,” Bull. Soc. Géol. France, 2e sée. t. xiii. p. 226 (1855–1856).Google Scholar

page 290 note 6 “Sopra i depositi di sal gemma e sulle acque salifere del Volterrano,” Ann. Univ. Tosc. Sci. Cosm. Pisa, t. vii. p. 27 (1862).Google Scholar

page 290 note 7 “Studi stratigrafici e paleontologici sull' Infralias nelle montagne del Golfo della Spezia,” Mem. Accad. Bologna, t. i. p. 247.Google Scholar

page 290 note 8 “Sulla Geologia dell' Italia centrale,” 1864.

page 292 note 1 For Messrs. Garrigou and Leymerie's spirited controversy, see Comptes Rendus. t. lxxviii. p. 1629, t. lxxix. pp. 53, 145, and 328.Google Scholar