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Stanton, R. L. (1984) The direct derivation of cordierite from a clay-chlorite precursor; evidence from the Geco Mine, Manitouwadge, Ontario. Economic Geology, 79 (6) 1245-1264 doi:10.2113/gsecongeo.79.6.1245

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Reference TypeJournal (article/letter/editorial)
TitleThe direct derivation of cordierite from a clay-chlorite precursor; evidence from the Geco Mine, Manitouwadge, Ontario
JournalEconomic Geology
AuthorsStanton, R. L.Author
Year1984 (October 1)Volume79
Page(s)1245-1264Issue6
PublisherSociety of Economic Geologists
DOIdoi:10.2113/gsecongeo.79.6.1245Search in ResearchGate
Mindat Ref. ID229242Long-form Identifiermindat:1:5:229242:1
GUID5dea4fce-3c9a-4946-9d57-26963b2a7d5a
Full ReferenceStanton, R. L. (1984) The direct derivation of cordierite from a clay-chlorite precursor; evidence from the Geco Mine, Manitouwadge, Ontario. Economic Geology, 79 (6) 1245-1264 doi:10.2113/gsecongeo.79.6.1245
Plain TextStanton, R. L. (1984) The direct derivation of cordierite from a clay-chlorite precursor; evidence from the Geco Mine, Manitouwadge, Ontario. Economic Geology, 79 (6) 1245-1264 doi:10.2113/gsecongeo.79.6.1245
In(1984, October) Economic Geology Vol. 79 (6) Society of Economic Geologists


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