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 |
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Sprache: | eng |
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