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Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma

✍ Scribed by Nick Petford; Kerry Gallagher


Book ID
117093841
Publisher
Elsevier Science
Year
2001
Tongue
English
Weight
703 KB
Volume
193
Category
Article
ISSN
0012-821X

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Contamination of mafic magma by partial
✍ T. Wenzel; L. P. Baumgartner; G. E. Brügmann; E. G. Konnikov; E. V. Kislov; 📂 Article 📅 2001 🏛 John Wiley and Sons 🌐 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