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The Granite Controversy

Published online by Cambridge University Press:  01 May 2009

Doris L. Reynolds
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Extract

This year, the 150th anniversary of Hutton's death, we are particularly reminded of the lively struggle of the eighteenth century between Vulcanists and Neptunists; the more so since that struggle finds its counterpart to-day in the divergence of opinion between two schools of petrology whose respective members might aptly be called Magmatists and Transformists. Much of the disagreement between the modern opponents arises from a belief on the part of the Magmatists that Hutton proved the magmatic origin of granite, and, in addition, the disagreement is probably strengthened by a misunderstanding of the views held by Transformists, and by lack of knowledge or experience of the evidence on which they base their conclusions. Indeed, Transformists might be tempted to preface their writings with the following very apposite quotation from Werner (1781):—

“I must here present a request to all who would judge of this theory, or communicate their sentiments on it to the public, viz. to begin by reading through the whole treatise, and then to peruse it a second time, with attention. Such a request will not only appear strange to many persons, but even superfluous ; I find myself, however, under the necessity of making it from the manner followed by some individuals with my book on the external characters of fossils. They have often represented me as saying quite the contrary of what I have expressly written. This may have been done by some, through design, but in by far the greater number of instances, it has happened from that work not having been read through ; and in this manner the public has frequently been led into an error, at least for some time.”

Type
Articles
Information
Geological Magazine , Volume 84 , Issue 4 , August 1947 , pp. 209 - 223
Copyright
Copyright © Cambridge University Press 1947

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References

REFERENCES

Backlund, H. G., 1937. Die Umgrenzung der Svekofenniden. Bull. Geol. Inst. Upsala, 27, 219–269.Google Scholar
Backlund, H. G., 1946. The Granitization Problem. Geol. Mag., 83, 105–117.CrossRefGoogle Scholar
van Bemmelen, R. W., 1938. On the Origin of the Pacific Magma types in the Volcanic Inner-arc of the Soenda Mountain system. Mijnbouw en Geologie, 4, No. 1, 1–14.Google Scholar
Bowen, N. L., 1910. Diabase and Granophyre of the Gowganda Lake District, Ontario. Journ. Geol., 18, 658–674.CrossRefGoogle Scholar
Bray, J. M., 1942. Spectroscopic distribution of Minor Elements in Igneous Rocks from Jamestown, Colorado. Bull. Geol. Soc. America, 53, 765–814.CrossRefGoogle Scholar
Bugge, J. A. W., 1946. The Geological importance of Diffusion in the Solid State. Norske Videnskaps-Akademi 1 Oslo. 1. Mat.-Nat. Klasse, 1945, No. 13, 5–59.Google Scholar
Desch, C. H., 1934. The Chemistry of Solids.Google Scholar
Fenner, C. N., 1937. A View of Magmatic Differentiation. Journ. Geol., 45, 158–168.CrossRefGoogle Scholar
Grout, F. F., 1941. Formation of Igneous-looking rocks by Metasomatism: a criticalReview and suggested Research. Bull. Geol. Soc. Amer., 52, 1525–1576.CrossRefGoogle Scholar
Holmes, A., 1936. Transfusion of Quartz Xenoliths in alkali basic and ultrabasic lavas, south-west Uganda. Min. Mag., 24, 408–420.Google Scholar
de Lapparent, J., 1941. Logique des minéraux du granite. Revue Scienti-fique, Nos. 5–6, 285–292.Google Scholar
Lonsdale, , Kathleen, , 1947. The Structure of Real Crystals. Science Progress, 35, 1–22.Google Scholar
Murray, J., 1802. A comparative View of the Huttonian and Neptunian Systems of Geology. Edinburgh.Google Scholar
Nockolds, S. R., 1934. The Production of Normal Rock Types by Contamination and their Bearing on Petrogenesis. Geol. Mag., 71, 31–9.CrossRefGoogle Scholar
Nockolds, S. R., 1941. The Garabal Hill-Glen Fyne Igneous Complex. Quart. Journ. Geol. Soc., 96, 451–511.CrossRefGoogle Scholar
Nockolds, S. R., 1947. The Granite Cotectic Curve. Geol. Mag., 84, 19–28.CrossRefGoogle Scholar
Nockolds, S. R., 1947. Crystallization of Plutonic and Hypabyssal Rocks. Geol. Mag., 84, 59–61.CrossRefGoogle Scholar
Playfair, J., 1802. Illustrations of the Huttonian Theory.CrossRefGoogle Scholar
Reynolds, , Doris, L., 1934. The Eastern end of the Newry Igneous Complex. Quart. Journ. Geol. Soc., 90, 585–636.CrossRefGoogle Scholar
Reynolds, , Doris, L., 1936. Demonstrations in Petrogenesis from Kiloran Bay, Colonsay. I. The Transfusion of Quartzite. Min. Mag., 24, 367–407.Google Scholar
Reynolds, , Doris, L., 1937. Contact Phenomena indicating a Tertiary Age for the Gabbros of the Slieve Gullion District. Proc. Geol. Assoc., 48, 247–275.CrossRefGoogle Scholar
Reynolds, , Doris, L., 1941. A Gabbro-Granodiorite Contact in the Slieve Gullion Area, and its Bearing on Tertiary Petrogenesis. Quart. Journ. Geol. Soc., 97, 1–38.CrossRefGoogle Scholar
Reynolds, , Doris, L., 1946. The sequence of Geochemical changes leading to Granitization. Quart. Journ. Geol. Soc., 102, 389–446.CrossRefGoogle Scholar
Reynolds, , Doris, L., 1947. The Association of Basic “Fronts’ with Granitization. Science Progress, 35, 205–219.Google Scholar
Richey, J. E., 1935. Further Evidence Concerning the Age of the Gabbros of the Slieve Gullion District. Proc. Geol. Assoc., 46, 487–492.CrossRefGoogle Scholar
Termier, P., 1910. Sur la genése des terrains cristallophylliens. C.R. XI International Geol. Cong., 587–595.Google Scholar
Tilley, C., 1947. Hercynian Fe-Mg Metasomatism in Cornwall. Geol. Mag., 84, 119.CrossRefGoogle Scholar
Werner, A. G., 1791. New Theory of the Formation of Veins. Translated by Anderson, C., 1809, Edinburgh.Google Scholar