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Offler, R., Shaw, S. (2006) Hornblende Gabbro Block in Serpentinite Mélange, Peel‐Manning Fault System, New South Wales, Australia: Lu‐Hf and U‐Pb Isotopic Evidence for Mantle‐Derived, Late Ordovician Igneous Activity. The Journal of Geology, 114 (2) 211-230 doi:10.1086/499572

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Reference TypeJournal (article/letter/editorial)
TitleHornblende Gabbro Block in Serpentinite Mélange, Peel‐Manning Fault System, New South Wales, Australia: Lu‐Hf and U‐Pb Isotopic Evidence for Mantle‐Derived, Late Ordovician Igneous Activity
JournalThe Journal of Geology
AuthorsOffler, R.Author
Shaw, S.Author
Year2006 (March)Volume114
Issue2
PublisherUniversity of Chicago Press
DOIdoi:10.1086/499572Search in ResearchGate
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Mindat Ref. ID163678Long-form Identifiermindat:1:5:163678:3
GUID0
Full ReferenceOffler, R., Shaw, S. (2006) Hornblende Gabbro Block in Serpentinite Mélange, Peel‐Manning Fault System, New South Wales, Australia: Lu‐Hf and U‐Pb Isotopic Evidence for Mantle‐Derived, Late Ordovician Igneous Activity. The Journal of Geology, 114 (2) 211-230 doi:10.1086/499572
Plain TextOffler, R., Shaw, S. (2006) Hornblende Gabbro Block in Serpentinite Mélange, Peel‐Manning Fault System, New South Wales, Australia: Lu‐Hf and U‐Pb Isotopic Evidence for Mantle‐Derived, Late Ordovician Igneous Activity. The Journal of Geology, 114 (2) 211-230 doi:10.1086/499572
In(2006, March) The Journal of Geology Vol. 114 (2) University of Chicago Press


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