Hostname: page-component-586b7cd67f-gb8f7 Total loading time: 0 Render date: 2024-11-26T10:46:15.219Z Has data issue: false hasContentIssue false
  • English
  • Français

The chemical composition and physical properties of the residual glass of the Kap Daussy tholeiite dike, east Greenland

Published online by Cambridge University Press:  14 March 2018

E. A. Vincent
E. A. Vincent*
Affiliation:
Durham Colleges in the University of Durham
Get access Rights & Permissions [Opens in a new window]

Extract

In the course of a petrological examination of some hundreds of specimens from the Tertiary coastal dike swarm of east Greenland, collected at various times by L. R. Wager and W. A. Deer, it was decided to investigate the nature of the residual glassy mesostasis of one of the olivine-tholeiites, in the hope that it might shed some light on the trend of differentiation of the magma responsible for the bulk of the rocks in the swarm. An account of the petrology of the swarm as a whole will be published in due course, but it was thought that a note on the chemical and physical properties of this glassy residuum might be worthy of independent publication, particularly as it provides an interesting comparison with the results of work carried out by Walker (1930, 1935) on the residual glass from one of the Upper Carboniferous tholeiites from central Scotland. The general features of the east Greenland coastal dike swarm have already been described by Wager and Deer (1938) and Wager (1947).

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 29 , Issue 208 , March 1950 , pp. 46 - 62
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1950

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

Anderson, (E.M.) and Radley, (E.G.), 1915. The pitchstones of Mull and their genesis. Quart. Journ. Geol. Soc. London, vol. 71, pp. 205–217.Google Scholar
Bailey, (E.B.), et al., 1924. Tertiary and post-Tertiary geology of Mull, Loch Aline and Oban. Mem. Geol. Surv. ('Mull Memoir.')Google Scholar
George, (W.O.), 1924. The relation of the physical properties of natural glasses to their chemical composition. Journ. Geol. Chicago, vol. 32, pp. 353–372.Google Scholar
Nockolds, (S.R.), 1941. The Garabal Hill-Glen Fyne igneous complex. Quart. Journ. Geol. Soc. London, vol. 96, pp. 451–51.. [M.A. 8 –164.]Google Scholar
Spencer, (L.J.), 1939. Tektites and silica-glass. Min. Mag., vol. 25, pp. 425–440.Google Scholar
Tilley, (C.E.), 1922. Density, refractivity, and composition relations of some natural glasses. Min. Mag., vol. 19, pp. 275–294.Google Scholar
Tomkeieff, (S.I.), 1929. A contribution to the petrology of the Whin Sill. Min. Mag., vol. 22, pp. 100–120.Google Scholar
Water, (L.R.), 1947. Geological investigations in east Greenland. Part IV. The stratigraphy and tectonics of Knud Rasmussens Land and the Kangerdlugssuaq region. Meddelelser om Gronland, vol. 134, no. 5.Google Scholar
Wager, (L.R.) and Deer, (W.A.), 1938. A dyke swarm and crustal flexure in east Greenland. Geol. Mag., vol. 75, pp. 39–46.Google Scholar
Wager, (L.R.) and Deer, (W.A.), 1939. Geological investigations in east Greenland. Part III. The petrology of the Skaergaard intrusion, Kangerdlugssuaq, east Greenland. Meddelelser om Gronland, vol. 105, no. 4. [M.A. 8–27.]Google Scholar
Walker, (F.), 1930. A tholeiitic phase of the quartz-dolerite magma of central Scotland. Min. Mag., vol. 22, pp. 368–376.Google Scholar
Walker, (F.), 1935. The late Palaeozoic quartz-doleFites and tholefitcs of Scotland. Min. Mag., vol. 24, pp. 131–159.Google Scholar
Walker, (F.), and Poldervaart, (A.), 1949. Karroo dolerites of the Union of South Africa. Bull. Geol. Soc. Amer., vol. 60, pp. 591–705. [M.A. 11–32.]Google Scholar
Washigton, (H.S.), 1917. Chemical analyses of igneous rocks. Prof. Paper U.S. Geol. Surv., no. 99. [M.A. 1–55.]Google Scholar