Ref.: Eur. Jour. Mineral. , 1994, 6, pp. 145-150.
Lamprophyric dykes closely associated with peraluminous granite intruded in the Eastern Cordillera of Southern Peru during Oligocene.
Located 1.5 km NE of Chili Palca Hacienda (70° 30' 48" W, 14° 17' 43" S).
The Chili Palca transitional lamproite is the product of mixing between olivine lamproite and peraluminous granite melts.
Mineral List:18 entries listed. 11 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!
