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It's a mineral found mostly in the farthest reaches of space vs one so common an exhaustive list of localities is nigh impossible as alloy #taenite faces off against clay #nontronite.
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ISHIKAWA, Hideo, SHIBANO, Terufumi (1974) 鹿児島県八瀬尾における四万十帯中のじゃ紋岩. The Journal of the Geological Society of Japan, 80 (10) 487-488 doi:10.5575/geosoc.80.487

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Reference TypeJournal (article/letter/editorial)
Title鹿児島県八瀬尾における四万十帯中のじゃ紋岩
JournalThe Journal of the Geological Society of Japan
AuthorsISHIKAWA, HideoAuthor
SHIBANO, TerufumiAuthor
Year1974Volume80
Issue10
PublisherThe Geological Society of Japan
DOIdoi:10.5575/geosoc.80.487Search in ResearchGate
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Mindat Ref. ID928246Long-form Identifiermindat:1:5:928246:3
GUID0
Full ReferenceISHIKAWA, Hideo, SHIBANO, Terufumi (1974) 鹿児島県八瀬尾における四万十帯中のじゃ紋岩. The Journal of the Geological Society of Japan, 80 (10) 487-488 doi:10.5575/geosoc.80.487
Plain TextISHIKAWA, Hideo, SHIBANO, Terufumi (1974) 鹿児島県八瀬尾における四万十帯中のじゃ紋岩. The Journal of the Geological Society of Japan, 80 (10) 487-488 doi:10.5575/geosoc.80.487
In(1974) The Journal of the Geological Society of Japan Vol. 80 (10) The Geological Society of Japan


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