Shallow crustal structure of eastern trans-Mexican volcanic belt: Gravity and magnetic constraints

Author:

Campos-Enríquez J.O.,Vázquez-Domínguez C.,Keppie J.D.,Quintero W.,Espinosa-Cardeña J.M.

Funder

Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México

National Autonomous University of Mexico

Publisher

Elsevier BV

Reference87 articles.

1. El sistema de fallas Taxco-San Miguel de Allende y la Faja Volcánica Trans-Mexicana, dos fronteras tectónicas del centro de México activas durante el Cenozoico;Alaniz-Alvares;Bol. Soc. Geol. Mex.,2005

2. Structural evolution of the Sierra de Juarez mylonitic complex, State of Oaxaca, Mexico;Alaniz-Álvarez;Rev. Mexicana de Ciencias Geol.,1994

3. Radiometric and kinematic evidence for Middle Jurassic strike-slip faulting in southern Mexico related to the opening of the Gulf of Mexico;Alaniz-Álvarez;Geology,1996

4. Basement faults deductions at a dumpsite using advanced analysis of gravity and magnetic anomalies, near Surface;Alatorre-Zamora;Geophysics,2020

5. Paleomagnetism and tectonics from the late Pliocene to late Pleistocene in the Xalapa monogenetic volcanic field, Veracruz, Mexico;Alva-Valdivia;GSA Bull.,2019

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