Hostname: page-component-848d4c4894-pftt2 Total loading time: 0 Render date: 2024-06-05T12:15:55.773Z Has data issue: false hasContentIssue false
  • English
  • Français

The Petrology of a Teschenite Sill at Landywood, Staffordshire

Published online by Cambridge University Press:  01 May 2009

M. E. Barton
M. E. Barton
Affiliation:
Dept. of Geology, University of Birmingham.
Get access Rights & Permissions [Opens in a new window]

Abstract

Borehole cores have been obtained of a basic igneous sill at Landywood, near Cannock, Staffordshire. This intrusion consists mainly of microteschenite with a zone of teschenite in the top half of the sill. Later parts of the parental magma of this intrusion were dryer and crystallized to give crinanite and analcite olivine dolerite. These later parts were not intruded in sufficient quantities to spread through the whole of the sill and were restricted to the vicinity of the feeding pipe. Extensive secondary replacement of plagioclase by chlorite and of pyroxene by carbonate occurs in the teschenitic parts of the sill and is ascribed to the action of water and carbon dioxide derived from the magma.

Type
Articles
Information
Geological Magazine , Volume 100 , Issue 6 , December 1963 , pp. 533 - 550
Copyright
Copyright © Cambridge University Press 1963

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

Barton, M. E., 1960. A Petrological Study of Two Basic Igneous Intrusions in the English West Midlands. Unpublished Ph.D. Thesis. University of Birmingham.Google Scholar
Batty, M. H., 1956. The Petrogenesis of a Spilitic Rock Series from New Zealand. Geol. Mag., 93, 89–110.CrossRefGoogle Scholar
Drever, H. I., and Johnston, R., 1958. The Lower Margin of the Shiant Isles Sill. Quart. J. Geol. Soc., London, 114, 343–365.CrossRefGoogle Scholar
SirFlett, J., 1929. The Easter Dalmeny Teschenite. Geol. Surv. Summ. Prog., 59–75.Google Scholar
SirFlett, J., 1930. The Blackness Teschenite. Geol. Surv. Summ. Prog., 39–45.Google Scholar
Fuller, R. E., 1950. Joint Cracks in the Diabase of the Palisades Sill, Bull. geol. Soc. Amer., 61, 1523.Google Scholar
Hunt, C. B., Averitt, P., and Miller, R. L., 1953. Geology and Geography of the Henry Mountains Region, Utah. U.S. Geol. Surv. Prof. Paper, No. 228.Google Scholar
Jaeger, J. C., 1957. Temperatures in the Neighbourhood of a Cooling Intrusive Sheet. Amer. J. Sci., 255, 306–318.CrossRefGoogle Scholar
Kennedy, G. C., 1955. Some Aspects of the Role of Water in Rock Melts. Geol. Soc. Amer., Special Paper, No. 62, 489–503.Google Scholar
Parry, V., 1937. The Broadlane Area. National Coal Board Report.Google Scholar
Tomkeieff, S., 1941. Metasomatism in the Basalt of Haddenrig Quarry near Kelso and the Veining of the Rocks Exposed there. Miner. Mag., 26, 45–59.Google Scholar
Tomkeieff, S. and Tesch, P., 1931. On a Dolerite in the Dutch Carboniferous. Geol. Mag., 68, 231–236.CrossRefGoogle Scholar
Vuagnat, M., 1953. Sur un Phenomene de Metasomatisme dans les Roches Vertes du Montgenevre (Hautes Alpes). Bull. Soc. Franc. Min., 76, 438–450.Google Scholar
Wager, L. R., 1929. Metasomatism in the Whin Sill of the North of England, Part II, Hydrothermal Alteration by Juvenile Solutions. Geol. Mag., 66, 221–238.CrossRefGoogle Scholar
Wilshire, H. G., 1958. Alteration of Olivine and Orthopyroxene in Basic Lavas and Shallow Intrusions. Amer. Min., 43, 120–147.Google Scholar