Burial metamorphism has produced many secondary minerals in Tertiary volcanic and sedimentary rocks from western Viti Levu, Fiji. Secondary assemblages include: albiteepidote-chlorite-sphene, albite-sericite-chlorite-prehnite-pumpdlyite-quartz, rnordenite( ?)-quartz-celadonite, and chabazite with a phyllosilicate and any two of thomsonite, phillipsite, and analcime. The primary fabrics of the host rocks are usually unchanged. Mineralogical modification may have resulted from burial alone, or from a combination of burial and a regional elevation of temperature connected with Tertiary volcanism. Some samples of chabazite give an X-ray powder pattern with additional lines in the position of the strongest reflections of phillipsite. Only a single phase is optically identifiable in each case. © 1963, Taylor & Francis Group, LLC. All rights reserved.
CITATION STYLE
Crook, K. A. W. (1963). Burial Metamorphic Rocks From Fiji. New Zealand Journal of Geology and Geophysics, 6(5), 681–704. https://doi.org/10.1080/00288306.1963.10423607
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