The shallow structure of Los Humeros and Las Derrumbadas geothermal fields, Mexico

Campos-Enríquez, J. O.; Monroy, Víctor Hugo Garduño

doi:10.1016/0375-6505(87)90038-1

Cited by 37 publications

(23 citation statements)

References 7 publications

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“…These extensional structures have been described as preferential pathways for the Eocene-Oligocene magmatic intrusions preceding the onset of the TMVB volcanism and, later, for the emplacement of Plio-Quaternary volcanoes, like the NNE-SSW Pico de Orizaba-Cofre de Perote volcanic chain (e.g. Campos-Enriquez and Garduno-Monroy, 1987;Lopez-Hernandez, 1995;Gutierrez-Negrin and Izquierdo-Montalvo, 2010).…”

Section: Background: Geological and Structural Setting Of The Lhvcmentioning

confidence: 97%

“…This orogenic process produced low-grade regional metamorphism on the sedimentary sequence (e.g. Campos-Enriquez and Garduno-Monroy, 1987;LopezHernandez, 1995;English and Johnston, 2004;Gutierrez-Negrin and Izquierdo-Montalvo, 2010). Second, one or more not well defined Eocene-Pliocene extensional and transtensional phases produced N-S to NE-striking normal faults (e.g.…”

Section: Background: Geological and Structural Setting Of The Lhvcmentioning

confidence: 98%

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Structural analysis and thermal remote sensing of the Los Humeros Volcanic Complex: Implications for volcano structure and geothermal exploration

Norini

Groppelli

Sulpizio

et al. 2015

Journal of Volcanology and Geothermal Research

208

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Section: Background: Geological and Structural Setting Of The Lhvcmentioning

confidence: 97%

Section: Background: Geological and Structural Setting Of The Lhvcmentioning

confidence: 98%

Structural analysis and thermal remote sensing of the Los Humeros Volcanic Complex: Implications for volcano structure and geothermal exploration

Norini

Groppelli

Sulpizio

et al. 2015

Journal of Volcanology and Geothermal Research

208

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“…A partir de 1980, con los estudio de Verma y López (1982), De la Cruz-Martínez (1983), Ferriz y Mahood (1984), Ferríz (1985), Campos-Enríquez y Garduño-Monroy (1987), Carrasco (1997) y Martínez-Serrano (2000), el estudio geológico de la zona cambia radicalmente al centrarse ahora en la evolución del CVLH, abordando el estudio de las unidades litológicas volcánicas y fuentes 1. Generalidades…”

Section: Antecedentesunclassified

“…los mas importantes : Ferriz, 1982: Ferriz, , 1985Verma y López, 1982;De la Cruz-Martínez, 1983;Ferríz y Mahood, 1984;Campa, 1985;Campos-Enríquez y Garduño-Monroy, 1987;Lugo-Hubp. 1999;Lugo-Hubp, et al, 2001y Ángeles y Sánchez, 2002.…”

unclassified

Estudio geológico para entender los procesos de remoción en masa en la región de Zacapoaxtla, Puebla, Mexico

Madrigal¹,

Monroy²,

Ayala³

2007

BSGM

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“…The Libres-Oriental basin volcanic field is limited on the east by the large (21 x 16 km) Los Humeros Caldera (Ferriz, 1984;Campos-Enriquez & Garduño-Monroy, 1987;Carrasco-Núñez & Branney, 2005), which is located 45 km southeast of Zapotitlán de Méndez (Fig. 1A).…”

Section: Cave Location and Geological Settingmentioning

confidence: 99%

Timing of speleogenesis of Las Karmidas Cave (Mexico): first description of pseudokarst developed in ignimbrite

Aliaga-Campuzano

López‐Martínez

Dávila-Harris

et al. 2017

IJS

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Abstract:Las Karmidas Cave (Puebla State, Mexico) is an unusual type of pseudokarstic cavity generated by piping and erosive processes within the contact of a diamicton and an overlying Quaternary ignimbrite. Morphological evidence suggests that the cave was developed in two stages: a phreatic stage and a vadose stage. The latter was characterized by the formation of carbonate speleothems. The absolute upper-age limit for the cave (168 +7.1/-7.5 ka) was established by U-Th dating of zircons grains extracted from the overlying ignimbrite, whilst a minimum age for the transition from a phreatic to vadose regime (95.6 ± 2.1 ka) was constrained by U-Th dating of carbonate speleothems within the cave. The geochronological results indicate a very rapid evolution of this pseudokarstic system, and suggest that similar systems might evolve and degrade at a very fast pace; consequently, making them hard to be preserved. Despite this, and considering the rather common geological context in which this system was developed, it is likely that similar pseudokarstic systems are yet to be detected worldwide.pseudokarst, cave, speleogenesis, Xaltipan ignimbrite, Las Karmidas Cave

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The shallow structure of Los Humeros and Las Derrumbadas geothermal fields, Mexico

Cited by 37 publications

References 7 publications

Structural analysis and thermal remote sensing of the Los Humeros Volcanic Complex: Implications for volcano structure and geothermal exploration

Structural analysis and thermal remote sensing of the Los Humeros Volcanic Complex: Implications for volcano structure and geothermal exploration

Estudio geológico para entender los procesos de remoción en masa en la región de Zacapoaxtla, Puebla, Mexico

Timing of speleogenesis of Las Karmidas Cave (Mexico): first description of pseudokarst developed in ignimbrite

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