Porosity evolution and mineral paragenesis during low-grade metamorphism of basaltic lavas at Teigarhorn
ABSTRACT. Low-grade alteration of basaltic lavas at Teigarhorn, eastern Iceland, resulted in three distinct stages of mineral paragenesis that correlate to events in the burial and intrusive history of Icelandic crust. Metasomatism and brittle deformation during the paragenetic stages dramatically a...
Main Authors: | , |
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Format: | Text |
Language: | English |
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1999
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.530.5769 http://earth.geology.yale.edu/~ajs/1999/06.1999.02Neuhoff.pdf |