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Breit, George N., Meunier, Jean-Dominique (1990) Fluid inclusion, delta 18 O, and 87 Sr/ 86 Sr evidence for the origin of fault-controlled copper mineralization, Lisbon Valley, Utah, and Slick Rock District, Colorado. Economic Geology, 85 (4) 884-891 doi:10.2113/gsecongeo.85.4.884

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Reference TypeJournal (article/letter/editorial)
TitleFluid inclusion, delta 18 O, and 87 Sr/ 86 Sr evidence for the origin of fault-controlled copper mineralization, Lisbon Valley, Utah, and Slick Rock District, Colorado
JournalEconomic Geology
AuthorsBreit, George N.Author
Meunier, Jean-DominiqueAuthor
Year1990 (July 1)Volume85
Page(s)884-891Issue4
PublisherSociety of Economic Geologists
DOIdoi:10.2113/gsecongeo.85.4.884Search in ResearchGate
Mindat Ref. ID228367Long-form Identifiermindat:1:5:228367:2
GUIDe0e81439-d76b-4a42-87a5-5fc079b6c09c
Full ReferenceBreit, George N., Meunier, Jean-Dominique (1990) Fluid inclusion, delta 18 O, and 87 Sr/ 86 Sr evidence for the origin of fault-controlled copper mineralization, Lisbon Valley, Utah, and Slick Rock District, Colorado. Economic Geology, 85 (4) 884-891 doi:10.2113/gsecongeo.85.4.884
Plain TextBreit, George N., Meunier, Jean-Dominique (1990) Fluid inclusion, delta 18 O, and 87 Sr/ 86 Sr evidence for the origin of fault-controlled copper mineralization, Lisbon Valley, Utah, and Slick Rock District, Colorado. Economic Geology, 85 (4) 884-891 doi:10.2113/gsecongeo.85.4.884
In(1990, July) Economic Geology Vol. 85 (4) Society of Economic Geologists


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