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Ryan, P. C. (1997) The Chemical Composition of Serpentine/Chlorite in the Tuscaloosa Formation, United States Gulf Coast: EDX vs. XRD Determinations, Implications for Mineralogic Reactions and the Origin of Anatase. Clays and Clay Minerals, 45 (3) 339-352 doi:10.1346/ccmn.1997.0450305

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Reference TypeJournal (article/letter/editorial)
TitleThe Chemical Composition of Serpentine/Chlorite in the Tuscaloosa Formation, United States Gulf Coast: EDX vs. XRD Determinations, Implications for Mineralogic Reactions and the Origin of Anatase
JournalClays and Clay Minerals
AuthorsRyan, P. C.Author
Year1997Volume45
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1346/ccmn.1997.0450305Search in ResearchGate
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Mindat Ref. ID147265Long-form Identifiermindat:1:5:147265:7
GUID0
Full ReferenceRyan, P. C. (1997) The Chemical Composition of Serpentine/Chlorite in the Tuscaloosa Formation, United States Gulf Coast: EDX vs. XRD Determinations, Implications for Mineralogic Reactions and the Origin of Anatase. Clays and Clay Minerals, 45 (3) 339-352 doi:10.1346/ccmn.1997.0450305
Plain TextRyan, P. C. (1997) The Chemical Composition of Serpentine/Chlorite in the Tuscaloosa Formation, United States Gulf Coast: EDX vs. XRD Determinations, Implications for Mineralogic Reactions and the Origin of Anatase. Clays and Clay Minerals, 45 (3) 339-352 doi:10.1346/ccmn.1997.0450305
In(1997) Clays and Clay Minerals Vol. 45 (3) Springer Science and Business Media LLC


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