Microscopic fabric of a refolded schist from Eastern Otago, New Zealand
نویسندگان
چکیده
منابع مشابه
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: New Zealand Journal of Geology and Geophysics
سال: 1967
ISSN: 0028-8306,1175-8791
DOI: 10.1080/00288306.1967.10428196