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The Contact Metamorphism and Related Phenomena in the Neighbourhood of Marulan, New South Wales

Published online by Cambridge University Press:  01 May 2009

G. D. Osborne
G. D. Osborne
Affiliation:
University of Sydney
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Extract

1. The contact metamorphic effects produced by the intrusion of quartz-monzonite into the Silurian limestone of the Marulan district, New South Wales, are described.

2. The rocks are divided broadly into marbles, hornfelses, skarns, and hybrid diopside-rocks. The first two groups are interpreted as being due to the recrystallization of limestone containing impurities which have reacted with the lime of the sediments to give lime-silicates and certain other minerals. The view is taken that only a very minor amount of pneumatolytic metamorphism followed the main thermal change. The skarns are shown to be due to the metasomatic replacement of recrystallized limestone by magmatic solutions rich in iron and silica, which were also responsible for the deposition of iron-oxides in cracks.

The hybrid rocks are explained as developing from limited marginal assimilation of limestone by the quartz-monzonite magma.

Type
Original Articles
Information
Geological Magazine , Volume 68 , Issue 7 , July 1931 , pp. 289 - 314
Copyright
Copyright © Cambridge University Press 1931

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References

page 289 note 1 Proc. Linn. Soc. N.S.W., xxxiv, 1909, 782–808.Google Scholar

page 289 note 2 Proc. Linn. Soc. N.S.W., xxxi, 1906, 546–54.Google Scholar

page 291 note 1 Communication from Professor W. R. Browne, of Sydney.

page 292 note 1 Geol. Surv. N.S.W., Mineral Resources, No. 25, 1919, 354.Google Scholar

page 295 note 1 α′ and γ′ refer respectively to the least and greatest indices determined approximately by the Schroeder-Becke Immersion method.Google Scholar

page 296 note 1 von Eckermann, H., The Rocks and Contact Minerals of the Mansjö Mountain, Stockholm, 1922, 373.Google Scholar

page 297 note 1 Vid. Selsk. Skrifter, 1911, No. 1, 439–44.Google Scholar

page 297 note 2 Bull. de la Soc. des Sciences, Bukarest, ix, 1900, 61.Google Scholar

page 298 note 1 Mikroscopische Physiographie, 5th Edition, Stuttgart, 1925, 132.Google Scholar

page 298 note 2 Geol. Fören. Förh. Stockholm, Nov—Dec., 1923, 497–8.Google Scholar

page 298 note 3 Bell. Dept. Geol. Univ. California, 1917, 327.Google Scholar Amer. Min., x, 1925, 97.Google Scholar

page 300 note 1 Amer. Journ. Sci., xl, 1915, 33.Google Scholar

page 301 note 1 Geol. Mag., LVII, 1920, 453.Google Scholar

page 304 note 1 Geol. Fören. Stockholm Förhand., 1923, Nov—Dec., 501.Google Scholar

page 305 note 1 Bergeat, A., Neues Jahrbuch, Beil. Band. xxviii, 1909, 421–572.Google Scholar

page 305 note 2 H. von Eckermann, loc. cit.

page 305 note 3 Eskola, P., Bull. Comm. Geol. Finland, 1914, No. 40, 253, 252–6.Google Scholar

page 307 note 1 Journ. Geol., xxx, 1922, 281–2.Google Scholar

page 307 note 2 Trans. Inst. Min. Met., xxxvii, 1928, 66–7.Google Scholar

page 310 note 1 Vid. Selsk. Skrifter, 1911, No. 1, 213.Google Scholar

page 310 note 2 Bull. Geol. Comm. Finland, 1914, 252.Google Scholar

page 310 note 3 Loc. cit., 214–16.Google Scholar

page 312 note 1 Geol. Fören. Stockholm. Förh., 1923, Nov—Dec., 524–6.Google Scholar

page 312 note 2 Trans. Inst. Min. Met., xxxvii, 1928, 69.Google Scholar