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Sheppard, Stephen, Krapež, Bryan, Zi, Jian-Wei, Rasmussen, Birger, Fletcher, Ian (2017) SHRIMP U–Pb zircon geochronology establishes that banded iron formations are not chronostratigraphic markers across Archean greenstone belts of the Pilbara Craton. Precambrian Research, 292. 290-304 doi:10.1016/j.precamres.2017.02.004

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Reference TypeJournal (article/letter/editorial)
TitleSHRIMP U–Pb zircon geochronology establishes that banded iron formations are not chronostratigraphic markers across Archean greenstone belts of the Pilbara Craton
JournalPrecambrian Research
AuthorsSheppard, StephenAuthor
Krapež, BryanAuthor
Zi, Jian-WeiAuthor
Rasmussen, BirgerAuthor
Fletcher, IanAuthor
Year2017 (May)Volume292
PublisherElsevier BV
URL
DOIdoi:10.1016/j.precamres.2017.02.004Search in ResearchGate
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Mindat Ref. ID707809Long-form Identifiermindat:1:5:707809:9
GUID0
Full ReferenceSheppard, Stephen, Krapež, Bryan, Zi, Jian-Wei, Rasmussen, Birger, Fletcher, Ian (2017) SHRIMP U–Pb zircon geochronology establishes that banded iron formations are not chronostratigraphic markers across Archean greenstone belts of the Pilbara Craton. Precambrian Research, 292. 290-304 doi:10.1016/j.precamres.2017.02.004
Plain TextSheppard, Stephen, Krapež, Bryan, Zi, Jian-Wei, Rasmussen, Birger, Fletcher, Ian (2017) SHRIMP U–Pb zircon geochronology establishes that banded iron formations are not chronostratigraphic markers across Archean greenstone belts of the Pilbara Craton. Precambrian Research, 292. 290-304 doi:10.1016/j.precamres.2017.02.004
In(2017) Precambrian Research Vol. 292. Elsevier BV


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