STILPNOMELANE CO-EXISTING WITH BIOTITE IN A RYOKE METAMORPHIC ROCK

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Reactions leading to the formation and breakdown of stilpnomelane in the Otago Schist, New Zealand

Semi-pelitic rocks ranging in grade from the prehnite–pumpellyite to the greenschist facies from southeastern Otago, New Zealand, have been investigated in order to evaluate the reactions leading to formation and breakdown of stilpnomelane. Detrital grains of mica and chlorite along with fine-grained authigenic illite and chlorite occur in lower-grade rocks with compactional fabric parallel to ...

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ژورنال

عنوان ژورنال: The Journal of the Geological Society of Japan

سال: 1966

ISSN: 0016-7630,1349-9963

DOI: 10.5575/geosoc.72.543