Vârful Cornetu
High-temperature skarns from Cornet Hill are developed at the contact between a quartz monzonitic – monzodioritic body of Paleocene – Ypresian age and Tithonian limestones. The skarns have undergone a late metasomatic event, and subsequent hydrothermal and weathering overprints.
References
- The Canadian Mineralogist 39, 1405-1434 (2001)
- Marincea, Ş., Bilal, E., Verkaeren, J., Pascal, M.-L., and Fonteilles, M. (2001): Superimposed paragenesis in spurrite-, tilleyite- and gehlenite-bearing skarns from Cornet Hill, Apuseni Mountains, Romania. Canadian Mineralogist 39, 1435-1453.
Mineral List
41 entries listed. 33 valid minerals.
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