Ch'iyar Qullu (Oruro)
Volcano in Bolivia
This article is about the mountain in the Ladislao Cabrera Province, Oruro Department, Bolivia. For other uses, see
Ch'iyar Qullu .
Ch'iyar Qullu (Aymara ch'iyara black, qullu mountain,[ 3] "black mountain", also spelled Chiar Kkollu ) is a volcanic centre in Bolivia . It is located in the Oruro Department , Ladislao Cabrera Province , Salinas de Garci Mendoza Municipality, northeast of Salinas de Garci Mendoza , near a maar named Jayu Quta ("salt lake").[ 4]
It is a sill formed from primitive phyric alkali basalt that closely resembles ocean island basalt in composition and now appears as a hill. The rocks contain augite and olivine and the eruption site coincides with a local lineament[ 2] [ 5] and is of Miocene age,[ 6] with dates of 22.51±0.45 mya by Ar-Ar dating and 25.2±0.5 mya by K-Ar dating .[ 5] The Ch'iyar Qullu magmas are Central Andes intraplate magmas and originate from the upper mantle .[ 7]
References
^ Pierre Soler, Gabriel Carlier, Michel G. Bonhomme, Michel FornariFORNARI, Field Observations and K-Ar DAting of the Cerro Chiar Kkollu (Southern Altiplano, Bolivia), Second ISAG, Oxford (UK), 21-23/9/1993 (see coordinates and sketch map)
^ a b Davidson, Jon P.; de Silva, Shanaka L. (1992). "Volcanic rocks from the Bolivian Altiplano: Insights into crustal structure, contamination, and magma genesis in the central Andes". Geology . 20 (12): 1127. Bibcode :1992Geo....20.1127D . doi :10.1130/0091-7613(1992)020<1127:VRFTBA>2.3.CO;2 .
^ Radio San Gabriel, "Instituto Radiofonico de Promoción Aymara" (IRPA) 1993, Republicado por Instituto de las Lenguas y Literaturas Andinas-Amazónicas (ILLLA-A) 2011, Transcripción del Vocabulario de la Lengua Aymara, P. Ludovico Bertonio 1612 (Spanish-Aymara-Aymara-Spanish dictionary)
^ "Salinas de Garco Mendoza" . INE, Bolivia. Archived from the original on January 27, 2016. Retrieved January 13, 2016 .
^ a b Davidson, Jon P.; de Silva, Shanaka L. (April 1995). "Late Cenozoic magmatism of the Bolivian Altiplano". Contributions to Mineralogy and Petrology . 119 (4): 387– 408. Bibcode :1995CoMP..119..387D . doi :10.1007/BF00286937 . S2CID 140667305 .
^ McLeod, C. L.; Davidson, J. P.; Nowell, G. M.; de Silva, S. L. (26 March 2012). "Disequilibrium melting during crustal anatexis and implications for modeling open magmatic systems" (PDF) . Geology . 40 (5): 435– 438. Bibcode :2012Geo....40..435M . doi :10.1130/G33000.1 .
^ Mazzuoli, R.; Vezzoli, L.; Omarini, R.; Acocella, V.; Gioncada, A.; Matteini, M.; Dini, A.; Guillou, H.; Hauser, N.; Uttini, A.; Scaillet, S. (7 November 2008). "Miocene magmatism and tectonics of the easternmost sector of the Calama-Olacapato-El Toro fault system in Central Andes at 24 S: Insights into the evolution of the Eastern Cordillera" (PDF) . Geological Society of America Bulletin . 120 (11– 12): 1493– 1517. Bibcode :2008GSAB..120.1493M . doi :10.1130/B26109.1 .