Geology and evolution of the Late Pleistocene-Holocene La Primavera caldera complex, western Trans-Mexican Volcanic Belt

La Primavera caldera is located in the western part of the Trans-Mexican Volcanic Belt. The landscape is represented by caldera-rim, intra-caldera, and extra-caldera domes and volcanoes associated with pyroclastic, lacustrine, and volcaniclastic deposits, all of which reflect a complex caldera evolution. La Primavera erupted ∼95 ky ago through the emission of the Tala ignimbrite, resulting in an 11-km wide caldera. Post-caldera activity occurred along the caldera ring-fault and within the depression, interacting with lacustrine sedimentation (93.8-71 ky) and outside the caldera rim with the development of the San Miguel, Planillas, Tajo, and Colli volcanoes (92-6.4 ky). The map (scale 1:30,000) comprises an area of 856 km² based on an ArcMap dataset. It incorporates previous studies and new field data, offering new insights to decision-making authorities for the careful planning of urban and park developments.

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Publication Details

Journal
Journal of Maps
Published
2026-04-13
DOI
https://doi.org/10.1080/17445647.2026.2650939
Primary Topic
Geological and Tectonic Studies in Latin America
Type
article
Field-Weighted Citation Impact
0.00

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article

Geology and evolution of the Late Pleistocene-Holocene La Primavera caldera complex, western Trans-Mexican Volcanic Belt

José Luis Arce, Denis Ramón Avellán, Delphine Sourisseau, J. L. Macías et al.
Journal of Maps
Geological and Tectonic Studies in Latin America
article

Geology and evolution of the Late Pleistocene-Holocene La Primavera caldera complex, western Trans-Mexican Volcanic Belt

José Luis Arce, Denis Ramón Avellán, Delphine Sourisseau, J. L. Macías, Antonio Pola, Juan Pablo Bernal, Yam Zul Ernesto Ocampo-Díaz, Ricardo Saucedo-Girón, F. García-Tenorio, Juan Manuel Sánchez-Núñez, Giovanni Sosa-Ceballos, Guillermo Cisneros, Pedro Corona-Chávez, Zareth Tinoco-Murillo
article en

Abstract

La Primavera caldera is located in the western part of the Trans-Mexican Volcanic Belt. The landscape is represented by caldera-rim, intra-caldera, and extra-caldera domes and volcanoes associated with pyroclastic, lacustrine, and volcaniclastic deposits, all of which reflect a complex caldera evolution. La Primavera erupted ∼95 ky ago through the emission of the Tala ignimbrite, resulting in an 11-km wide caldera. Post-caldera activity occurred along the caldera ring-fault and within the depression, interacting with lacustrine sedimentation (93.8-71 ky) and outside the caldera rim with the development of the San Miguel, Planillas, Tajo, and Colli volcanoes (92-6.4 ky). The map (scale 1:30,000) comprises an area of 856 km² based on an ArcMap dataset. It incorporates previous studies and new field data, offering new insights to decision-making authorities for the careful planning of urban and park developments.

Journal of MapsVol. 22(1)
Universidad Michoacana de San Nicolás de Hidalgo (MX), Autonomous University of San Luis Potosí (MX), Instituto Politécnico Nacional (MX), Universidad Nacional Autónoma de México (MX)
Centro Mexicano de Innovación en Energía Geotérmica, Consejo Nacional de Ciencia y Tecnología, Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México
Openalex Percentile: Top 18%
Geological and Tectonic Studies in Latin America
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