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.
The above list contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please
register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
Mineral and Locality Search
