Ubinas: the evolution of the historically most active volcano in southern Peru

@article{Thouret2005UbinasTE,
  title={Ubinas: the evolution of the historically most active volcano in southern Peru},
  author={Jean-Claude Thouret and Marco Rivera and Gerhard W{\"o}rner and Marie C. Gerbe and Anthony Finizola and Michel Fornari and Katherine Gonzales},
  journal={Bulletin of Volcanology},
  year={2005},
  volume={67},
  pages={557-589}
}
Ubinas volcano has had 23 degassing and ashfall episodes since A.D. 1550, making it the historically most active volcano in southern Peru. Based on fieldwork, on interpretation of aerial photographs and satellite images, and on radiometric ages, the eruptive history of Ubinas is divided into two major periods. Ubinas I (Middle Pleistocene >376 ka) is characterized by lava flow activity that formed the lower part of the edifice. This edifice collapsed and resulted in a debris-avalanche deposit… 
The historical (218 ± 14 aBP) explosive eruption of Tutupaca volcano (Southern Peru)
The little known Tutupaca volcano (17° 01′ S, 70° 21′ W), located at the southern end of the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption during historical
Eruptive history of Incahuasi, Falso Azufre and El Cóndor Quaternary composite volcanoes, southern Central Andes
Volcanoes can stay dormant for much longer than 10 ka and hence many Quaternary volcanoes lacking Holocene activity have the potential to become active. Reconstructing the eruptive histories of these
...
...

References

SHOWING 1-10 OF 51 REFERENCES
Geology of El Misti volcano near the city of Arequipa, Peru
Approximately 750 000 people live at risk in the city of Arequipa, whose center lies 17 km from the summit (5820 masl [meters above sea level]) of the active El Misti volcano. The composite edifice
The Nevados de Payachata volcanic region (18°S/69°W, N. Chile)
Subduction-related volcanism in the Nevados de Payachata region of the Central Andes at 18°S comprises two temporally and geochemically distinct phases. An older period of magmatism is represented by
The Nevados de Payachata volcanic region (18°S/69°W, N. Chile) II. Evidence for widespread crustal involvement in Andean magmatism
Volcanism extending over 11 Ma is represented in the rocks of the Nevados de Payachata region, culminating in the formation of two large composite stratocones within the last 500 000 years.
Role of magma mixing in the petrogenesis of tephra erupted during the 1990–98 explosive activity of Nevado Sabancaya, southern Peru
The Nevado Sabancaya in southern Peru has exhibited a persistent eruptive activity over eight years following a violent eruption in May–June 1990. The explosive activity consisted of alternated
Intracrustal Derivation of Na-Rich Andesitic and Dacitic Magmas: An Example from Volcán Ollagüe, Andean Central Volcanic Zone
Andesitic and dacitic lavas erupted from Quaternary stratovolcanoes in the Central Volcanic Zone (CVZ) of the Andes have major and trace element compositions similar to proposed melts of subducted
U-series evidence for crustal involvement and magma residence times in the petrogenesis of Parinacota volcano, Chile
Abstract In this study, we present Th–U disequilibria as well as radiogenic and trace element data for recent volcanic rocks from the Nevados de Payachata volcano which erupted through ∼70 km of
Recent glacial history and paleoclimate of the Peruvian-Bolivian Andes
...
...