Hostname: page-component-78c5997874-ndw9j Total loading time: 0 Render date: 2024-11-07T20:07:00.330Z Has data issue: false hasContentIssue false
  • English
  • Français

Crystallization of basaltic magma as recorded by variation of crystal-size in dikes

Published online by Cambridge University Press:  14 March 2018

Helmut G. F. Winkler
Helmut G. F. Winkler*
Affiliation:
Department of Mineralogy and Petrography, University of Göttingen
Get access Rights & Permissions [Opens in a new window]

Extract

It is a familiar fact that in dikes, lava-flows, and sills the grain-size of the individual minerals normally varies according to the distance from the contacts. At or near the margins of the igneous body the grainsize is usually very much less than in the centre, and this phenomenon has been attributed to differences in the cooling-velocities at these spots. On the basis of measurements carried out by Queneau (8) the opinion seems to have been formed that the crystal-size always shows a progressive increase from the contacts towards the centre. This is not so, however, for as Lane (6) has shown, the crystal-size may increase to a maximum at a certain distance from the margin, and thereafter decrease again towards the centre of the intrusion. Apart from these investigations, carried out by Queneau and Lane, the only additioual quantitative data oil crystal-size variation known to the writer concerns a series of measurements made on an olivine-diabase by B. H. Dollen, under the direction of H. L. Alling.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 28 , Issue 205 , June 1949 , pp. 557 - 574
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1949

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

1. Alling, (H. L.). Interpretative petrology of igneous rocks. New York and London, 1936.Google Scholar
2. Barth, (T. F. W.). The crystallization process of basalt. Amer. Journ. Sci., 1936, ser. 5, vol. 31, pp. 321–351 (p. 328). [M.A. 6–295.]CrossRefGoogle Scholar
Barth, (T. F. W.) Kristallisationsvorgang eines basaltischen Magmas. In Barth, Correns, Eskola, Die Entstehung der Gesteine. Berlin, 1939, pp. 74–80. [M.A. 7–367.]Google Scholar
3. Bowen, (N. L.). Das ternäre System: Diopsid-Anorthit-Albit. Zeits. Anorgan- Chem., 1916, vol. 94, pp. 23–50.Google Scholar
4. Holmes, (A.) and Harwood, (H. F.). The tholeiite dikes of the north of England. Min. Mag., 1929, vol. 22, pp. 1–52.Google Scholar
5. Kennedy, (W. Q.). Trends of differentiation in basaltic magmas. Amer. Journ. Sci., 1933, ser. 5, vol. 25, pp. 239–256.Google Scholar
6. Lane, (A. C.). Die Korngrösse der Auvergnosen. Nachtrag zur Rosenbusch- Festschrift, Stuttgart 1906, pp. 1–19.Google Scholar
7. Lovering, (F. S.). Theory of heat conduction applied to geological problems. Bull. Geol. Soc. Amer., 1935, vol. 46, pp. 69–94.Google Scholar
8. Queneau, (A. L.). Size of grain in igneous rocks in relation to the distance from the cooling wall. School of Mines Quart. New York, 1902, vol. 23, pp. 181–195.Google Scholar
9. Teall, (J. J. H.). Petrological notes on some north-of-England dykes. Quart. Journ. Geol. Soc. London, 1884, vol. 40, pp. 209–247.CrossRefGoogle Scholar
10. Walker, (F.). The late Palaeozoic quartz-dolerites and tholeiites of Scotland. Min. Mag., 1935, vol. 24, pp. 131–159 (p. 155).Google Scholar
11. Winkler, (H. G. F.). Kristallgrösse und AbKühlung. Heidelberger Beitr. Min. Petr., 1947, vol. 1, pp. 86–104. [M.A. 10–322, 425.]Google Scholar
12. Winkler, (H. G. F.). Zusammenhang zwischen Kristallgrösse und Salbandabstand bei magmatischen Gang-Intrusionen. Heidelberger Beitr. Min. Petr., 1948, vol. 1, pp. 251–263. [M.A. 10–425.]Google Scholar