Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-09T20:41:44.129Z Has data issue: false hasContentIssue false
  • English
  • Français

Granite: Some Tectonic, Petrological, and Physico-Chemical Aspects

Published online by Cambridge University Press:  01 May 2009

Doris L. Reynolds
Doris L. Reynolds
Affiliation:
Grant Institute of Geology, West Mains Road, Edinburgh, 9.
Get access Rights & Permissions [Opens in a new window]

Abstract

Granites of the main movement-phase of an orogenic zone form an integral part of the tectonic pattern being characteristically located at the intersection of cross- and main-folds. Here, an older granitic core pierces upwards through the anticlinal vault to form a diapir-fold in which migmatization, synchronous with movement, leads to the evolution of granodiorite. At higher structural levels where pressure is lower K-granites occur. Only at sub-volcanic levels has evidence of melting been found.

Recent hydrothermal investigations, by Bowen and Tuttle, show that synthetic haplo-pitchstones which begin to crystallize at minimum temperatures become richer in K as pressure decreases. These results are closely comparable with evidence provided by the sub-volcanic K-microgranites (migmatized Caledonian granodiorite) of Slieve Gullion, but have no application to the granodiorites.

Type
Articles
Information
Geological Magazine , Volume 95 , Issue 5 , October 1958 , pp. 378 - 396
Copyright
Copyright © Cambridge University Press 1958

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Argand, E., 1916. Sur l'arc Alpes occidentals. Eclogae géol. Helvet., xiv, 145–191.Google Scholar
Backlund, H. G., 1943. Einblicke in das geologische Geschehen des Präkambriums. Geol. Rundsch., xxxiv, 79–148.CrossRefGoogle Scholar
Backlund, H. G. 1950. Some observations on homogenization and on geochemical discontinuities in granitic areas. Internal. Geol. Cong., 1948, 18th session, Gt. Britain, Pt. iii, 31–144.Google Scholar
Barbeau, J., and Gèze, B., 1957. Les coupoles granitiques et rhyolitiques de la région de Fort-Lamy (Tchad). Bull. Soc. géol. France, vii, 341–351.Google Scholar
Barth, T. F. W., 1955. Température de formation de certains granites Précambriens de Norvège mèridionale. International Colloquium. Science de la Terre. Annales de l'École Nationale supérieure, Nancy, 119–129.Google Scholar
Bowen, N. L., 1954. Experiment as an aid to the understanding of the natural world. Proc. Acad. Nat. Sci. Philadelphia, cvi, 1–12.Google Scholar
Bowen, N. L. and Tuttle, O. F., 1951, 1952, 1953. In Annual report of the Director of the Geophysical Laboratory for the years 1950–51, 1951–52, 1952–53.Google Scholar
Chamberlin, T. C., 1897 and 1931. The method of multiple working hypotheses. Journ. Geol., v, 837–848, xxxix, 155–165.Google Scholar
Cook, A. H., and Murphy, T., 1952. Gravity survey of Ireland north of the line Sligo-Dundalk. Dublin Inst. Advanced Studies (School of cosmic physics), Geophysical Mem., 2, Pt. 4.Google Scholar
Eskola, P., 1949. The problem of mantled domes. Quart. Journ. Geol. Soc., civ, 461–676.Google Scholar
Eskola, P. 1950. The nature of metasomatism in the processes of granitization. Internal. Geol. Cong., 1948, 18th session Gt. Britain, pt. iii, 5–13.Google Scholar
Eskola, P., 1952. A discussion of domes and granites and ores. Compt. Soc. rendu. géol. Finlande, xxv, 125–144.Google Scholar
Eskola, P. 1955. About the granite problem and some Masters of the study of granite. Compt. Soc. rendu. géol. Finlande, 168. 117–130.Google Scholar
Eskola, P. 1956. Postmagmatic potash metasomatism of granite. Compt. rendu. Soc. géol. Finlande, xxix, 85–100.Google Scholar
Fourmarier, P., 1956. Les enseignments tire de l'étude de la schistosité dans les series plissées. Verhand. konink. Nederland. Geol. Mijnbou. genoot. (Brouwer volume), xvi, 114–130.Google Scholar
Goldschmidt, V. M., 1911. Die Kontaktmetamorphose im Kristianiagebeit. Videnskap. Skrift. 1, Mat.-Nat. Klasse, 11.Google Scholar
Goldschmidt, V. M. 1921. Die Injektionsmetamorphose im Stavangergebeite. Videnskap. Skrift. 10.Google Scholar
Haarmann, E., 1930. Die Oszillationstheorie. Eine Erklärung der Krusten-bewegungen von Erde und Mond, Stuttgart.Google Scholar
Haller, J., 1955. Der “ Zentrale Metamorphe Komplex ” von N.E.– Grönland. Medd. om. Gronland, 73, No. 3.Google Scholar
Hubbert, M. K., 1937. Theory of scale models as applied to the study of geologic structures. Bull. Geol. Soc. Amer., 48, 1459–1520.CrossRefGoogle Scholar
Hubbert, M. K. 1945. Strength of the earth. Bull. Amer. Assoc. Petroleum Geol., 29, 1630–1653.Google Scholar
Jung, J., and Roques, M., 1952. Introduction a l'étude zoneographique des formations cristallophylliennes. Bull. Serv. carte géeol. France, No. 235, L.Google Scholar
Morey, G. W., 1953. Hydrothermal synthesis. Journ. Amer. Ceramic Soc., 36, 279–85.CrossRefGoogle Scholar
Morey, G. W. and Hesselgesser, J. M., 1951. The solubility of some minerals in superheated steam at high pressures. Economic Geol., 46, 821–835.CrossRefGoogle Scholar
Morey, G. W. and Chen, W. T, 1955. The action of hot water on some feldspars. Amer. Min., 40, 996–1000.Google Scholar
Mrazec, L., 1910. Les gisements de pétrole. L'industrie du pétrole en Roumanie. Ministere de l'industrie et du commerce. Bucarest.Google Scholar
Perrin, R., 1957. Granites eutectiques ou métamorphiques ? Discussion d'études récentes. Bull. Soc. géol. France, 6 série, 7, 91–113.CrossRefGoogle Scholar
Read, H. H., 1951 and 1957. Metamorphism and granitization. Geol. Soc. South Africa, Annex to liv, and The granite controversy. Thomas Murby and Co., London, 339–373.Google Scholar
Reynolds, D. L., 1934. The eastern end of the Newry igneous complex. Quart. Journ. Geol. Soc., xc, 585–636.CrossRefGoogle Scholar
Reynolds, D. L. 1937. Contact phenomena indicating a Tertiary age for the gabbros of the Slieve Gullion district. Proc. Geol. Assoc., xlviii, 247–275.CrossRefGoogle Scholar
Reynolds, D. L. 1941. A gabbro-granodiorite contact in the Slieve Gullion area, and its bearing on Tertiary petrogenesis. Quart. Journ. Geol. Soc., xcvii, 1–38.CrossRefGoogle Scholar
Reynolds, D. L. 1947. The granite controversy. Geol. Mag., lxxxiv, 209–223.Google Scholar
Reynolds, D. L. 1949. Observations concerning granite. Geol.en Mijnbouw. lle jaargang, 241–263.Google Scholar
Reynolds, D. L. 1950. The transformation of Caledonian granodiorite to Tertiary granophyre on Slieve Gullion, Co. Armagh, N. Ireland. Inter. geol. Congress, 1948, 18th session, Gt. Britain, pt. iii, 20–30.Google Scholar
Reynolds, D. L. 1951. The geology of Slieve Gullion, Foughill and Carrickcarnan: an actualistic interpretation of a Tertiary gabbro-granophyre complex. Trans. Royal Soc. Edinb., lxii, 85–143.Google Scholar
Reynolds, D. L. 1952. Partially fused plagioclases in the rocks of Slieve Gullion. Trans. Edin. Geol. Soc., xv (Campbell volume), 280–296.Google Scholar
Reynolds, D. L. 1954. Fluidization as a geological process, and its bearings on the problem of intrusive granites. Amer. Journ. Sci., 252, 577–614.CrossRefGoogle Scholar
Reynolds, D. L. 1955. Calderas and ring-complexes. Verhand. konink. Nederland. Geol. Mijnbou. genoot. (Brouwer volume), xvi, 355–379.Google Scholar
Roques, M., 1941. Les schistes cristallins de la partie sud-ouest du Massif Central Français. Mem. Carte géol. détaillée, France.Google Scholar
Saucier, H., 1951. Quelques expériences sur la viscosité à haute température de verres ayant la composition d'un granite. Influence de la vapeur d'eau sous pression. Théses a la Faculté des Sciences de l'Universite de Paris.Google Scholar
Tuttle, O. F., 1955. l'origine et la classification des granites a la lumiere des études expérimentales dans le système NaAlSi3O8 – KalSi3O8 – SiO2 – H2O. International Colloquium. Sciences de la Terre. Annales de l'École Nationale supérieure, Nancy, 299–308.Google Scholar
Wegmann, C. E., 1930. Über Diapirismus (besonders im Grundgebirge). Bull. comm. géol. Finlande, 92, 58–76.Google Scholar
Wegmann, C. E. 1935 a. Preliminary report on the Caledonian orogeny in Christian X's land (north-east Greenland). Medd. om Grønland, 103, No. 3.Google Scholar
Wegmann, C. E. 1935 b. Zur Deutung der Migmatite. Geol. Rund., 26, 305–350.Google Scholar
Wyart, J., 1955. Cristallisation, par voie hydrothermale, d'un verre naturel et origine du granite. International Colloquium. Science de la Terre. Annales de l'École Nationale supérieure, Nancy, 177–188.Google Scholar