40Ar/39Ar geochronology and Pb isotopic evidence for the role of ridge subduction in generating orogenic gold mineralization in the Otago Schist Belt, New Zealand

Details 40Ar/39Ar geochronology and Pb isotopic evidence for the role of ridge subduction in generating orogenic gold mineralization in the Otago Schist Belt, New Zealand 40Ar/39Ar geochronology and Pb isotopic evidence for the role of ridge subduction in generating orogenic gold mineralization in the Otago Schist Belt, New Zealand

Jul 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008gecas..72q.655m&link_type=openurl

Geochimica et Cosmochimica Acta, Volume 72, Issue 12, p.A655

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