Re–Os isotopic constraints on magma mixing in the Peridotite Zone of the Stillwater Complex, Montana, USA

A study was undertaken to better constrain variation in Os initial isotopic ratios within and between chromite layers of the Peridotite Zone of the Stillwater Complex in Montana and in its source magmas, using Re-Os isotopic analysis of separated chromites from chromite layers and from silicate cumu...

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Veröffentlicht in:Contributions to mineralogy and petrology 2001-07, Vol.141 (4), p.446-457
Hauptverfasser: Horan, Mary F., Morgan, John W., Walker, Richard J., Cooper, Roger W.
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Sprache:eng
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Zusammenfassung:A study was undertaken to better constrain variation in Os initial isotopic ratios within and between chromite layers of the Peridotite Zone of the Stillwater Complex in Montana and in its source magmas, using Re-Os isotopic analysis of separated chromites from chromite layers and from silicate cumulate layers.
ISSN:0010-7999
1432-0967
DOI:10.1007/s004100100251