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Secondary ilvaite in a dolerite dyke from Rogaland, SW Norway

Published online by Cambridge University Press:  05 July 2018

Michael Barton  and
Manfred J. van Bergen
Michael Barton
Affiliation:
Vening-Meinesz Laboratory, Department of Geochemistry, Institute for Earth Sciences, State University of Utrecht, Budapestlaan 4, 3584 CD Utrecht, The Netherlands
Manfred J. van Bergen
Affiliation:
Vening-Meinesz Laboratory, Department of Geochemistry, Institute for Earth Sciences, State University of Utrecht, Budapestlaan 4, 3584 CD Utrecht, The Netherlands
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Abstract

Ilvaite is an alteration product of carbonate, which itself replaced clinopyroxene, in a Precambrian tholeiitic dyke. Additional secondary minerals are ferroactinolite, cummingtonite, chlorite, biotite, prehnite, and epidote. Microprobe analyses demonstrate that the ilvaite is close to the ideal end-member composition [CaFe22+Fe3+Si2O8 (OH)] and that only cummingtonites, Mg/(Mg+Fe2+) 0.77–0.39, and carbonates (solid solutions between calcite and dolomite, dolomite and ankerite, magnesite and siderite) show significant compositional variations. It is estimated that ilvaite formed at temperatures < 470 °C and at pressures < 2 kbar, probably during a low-grade metamorphic event (or events) associated with the Caledonian orogeny. The fluids involved in the alteration process contained both CO2 and H2O, initial fluids probably being richer in CO2 than later ones. Ilvaite may be more common in hydrothermally altered igneous rocks than previously supposed.

Type
Research Article
Information
Mineralogical Magazine , Volume 48 , Issue 348 , September 1984 , pp. 449 - 456
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1984

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