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The three geologic regions of Puebla State, Mexico

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  • Gilberto Silva-Romo
  • Claudia Cristina Mendoza-Rosales
  • Wendy Vanesa Morales Barrera
  • Yoalli Bianii Hernández-Marmolejo

Abstract

Puebla State, Mexico, stands out with its diverse geological features, ranging from Precambrian and Paleozoic crystalline basements to the Pliocene-Quaternary major volcanoes. It is divided into three distinct regions: the northern region with its predominantly marine successions, where outcrops a volcano-sedimentary marine succession aged between 171.3 ± 0.5 Ma and 168.6 ± 0.4 Ma; the central region, part of the Trans-Mexican Volcanic Belt; and the southern region, mainly characterized by a multitude of continental units on crystalline basements.BULLETS:Geological regionalization, geological provinces, genetic-chronostratigraphic units, key successions tableGeological records contrast between the northern and southern regionsFirst report of Middle Jurassic marine volcano-sedimentary succession in the Sierra Madre Oriental Range

Suggested Citation

  • Gilberto Silva-Romo & Claudia Cristina Mendoza-Rosales & Wendy Vanesa Morales Barrera & Yoalli Bianii Hernández-Marmolejo, 2024. "The three geologic regions of Puebla State, Mexico," Journal of Maps, Taylor & Francis Journals, vol. 20(1), pages 2428633-242, December.
    • Handle: RePEc:taf:tjomxx:v:20:y:2024:i:1:p:2428633
    DOI: 10.1080/17445647.2024.2428633
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