Contamination of mafic magma by partial
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T. Wenzel; L. P. Baumgartner; G. E. Brügmann; E. G. Konnikov; E. V. Kislov;
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Article
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2001
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John Wiley and Sons
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English
⚖ 337 KB
Mg‐skarns enclosed in dunite cumulates of the Neo‐Proterozoic Ioko‐Dovyren intrusion (northern Baikal region, Russia) can be traced to silica‐poor dolomitic host rock layers. The dominant minerals of the skarns are brucite (pseudomorph after periclase), forsterite and Cr‐poor spinel. Rapid heating o