Tourmaline in a low grade clastic metasedimentary rock. an example of the petrogenetic potential of tourmaline

Detrital tourmaline grains and their associated tourmaline overgrowths provide a means to unravel the provenance and petrogenetic history of low grade clastic metasedimentary rocks. Tourmaline growth stages may serve as a monitor of chemical reactions in low grade metamorphic rocks.

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Veröffentlicht in:Contributions to mineralogy and petrology 1992-11, Vol.112 (2-3), p.203-218
Hauptverfasser: HENRY, Darrell J, DUTROW, Barbara L
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Sprache:eng
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