Show simple item record

Title

Geology of the late Pliocene - Pleistocene Acoculco caldera complex, eastern Trans-Mexican Volcanic Belt (México)

dc.contributor.authorAvellán López, Denis Ramón
dc.contributor.authorMacías, José Luis
dc.contributor.authorLayer, Paul W.
dc.contributor.authorCisneros Maximo, Guillermo
dc.contributor.authorSánchez Nuñez, Juan Manuel
dc.contributor.authorGómez Vasconcelos, Martha Gabriela
dc.contributor.authorPola Villaseñor, Antonio
dc.contributor.authorSosa Ceballos, Giovanni
dc.contributor.authorGarcía Tenorio, Felipe
dc.contributor.authorReyes Agustín, Gabriela
dc.contributor.authorOsorio Ocampo, Lady Susana
dc.contributor.authorGarcía Sánchez, Laura
dc.contributor.authorMendiola, Irma Fabiola
dc.contributor.authorMarti, Joan
dc.contributor.authorLópez Loera, Héctor
dc.contributor.authorBenowitz, Jeff A.
dc.date.accessioned2020-03-25T01:26:38Z
dc.date.available2020-03-25T01:26:38Z
dc.date.issued2019
dc.identifier.citationDenis Ramón Avellán, José Luis Macías, Paul W. Layer, Guillermo Cisneros, Juan Manuel Sánchez Nuñez, Martha Gabriela Gómez-Vasconcelos, Antonio Pola, Giovanni Sosa-Ceballos, Felipe García-Tenorio, Gabriela Reyes Agustín, Susana Osorio-Ocampo, Laura García Sánchez, Irma Fabiola Mendiola, Joan Marti, Héctor López Loera & Jeff Benowitz (2019) Geology of the late Pliocene - Pleistocene Acoculco caldera complex, eastern Trans-Mexican Volcanic Belt (M̩xico), Journal of Maps, 15:2, 8-18, DOI: 10.1080/17445647.2018.1531075
dc.identifier.urihttp://hdl.handle.net/11627/5333
dc.description.abstract"We present a new 1:80,000-scale geologic map of the Acoculco caldera (Ac) located between the states of Puebla and Hidalgo in eastern Mexico. The map, encompassing an area of 856 km(2), is grounded on an ArcMap data set and is supported by nine new Ar-40/Ar-39 dates. The caldera lies upon Cretaceous limestones and Miocene to Pliocene volcanic rocks (13-3 Ma). The caldera consists of 31 lithostatrigraphic units formed between 2.7 and 0.06 Ma that include a wide variety of volcanic landforms (cinder cones, lava domes). The caldera has a semi-circular shape (18-16 km) bounded by the Atotonilco scarp to the north, the NW-SE Manzanito fault to the west, and scattered vents to the east and southern parts. The distribution of the Acoculco ignimbrite, the lithic breccia, and lacustrine sediments define the caldera ring fault. Late Pleistocene activity and pervasive hydrothermal alteration suggest a high geothermal potential in the area."
dc.publisherTaylor & Francis LTD
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectGeology
dc.subjectVolcanic stratigraphy
dc.subjectAcoculco caldera complex
dc.subjectPuebla
dc.subject.classificationGEOGRAFÍA
dc.titleGeology of the late Pliocene - Pleistocene Acoculco caldera complex, eastern Trans-Mexican Volcanic Belt (México)
dc.typearticle
dc.identifier.doihttps://doi.org/10.1080/17445647.2018.1531075
dc.rights.accessAcceso Abierto


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

Attribution-NonCommercial-NoDerivatives 4.0 Internacional
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 Internacional