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Gao, Pin; Santosh, M. (2020) Trace element and stable isotope characteristics of Algoma-type sulfidic banded iron formations from the Wutai Complex, central North China Craton. Ore Geology Reviews, 116. doi:10.1016/j.oregeorev.2019.103221

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Reference TypeJournal (article/letter/editorial)
TitleTrace element and stable isotope characteristics of Algoma-type sulfidic banded iron formations from the Wutai Complex, central North China Craton
JournalOre Geology Reviews
AuthorsGao, PinAuthor
Santosh, M.Author
Year2020 (January)Volume116
PublisherElsevier BV
DOIdoi:10.1016/j.oregeorev.2019.103221Search in ResearchGate
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Mindat Ref. ID236132Long-form Identifiermindat:1:5:236132:5
GUID0
Full ReferenceGao, Pin; Santosh, M. (2020) Trace element and stable isotope characteristics of Algoma-type sulfidic banded iron formations from the Wutai Complex, central North China Craton. Ore Geology Reviews, 116. doi:10.1016/j.oregeorev.2019.103221
Plain TextGao, Pin; Santosh, M. (2020) Trace element and stable isotope characteristics of Algoma-type sulfidic banded iron formations from the Wutai Complex, central North China Craton. Ore Geology Reviews, 116. doi:10.1016/j.oregeorev.2019.103221
In(2020) Ore Geology Reviews Vol. 116. Elsevier BV

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