Yuri Almaguer-Carmenates, José Alberto Batista-Rodríguez, Ramón Yosvanis Batista-Cruz, Felipe de Jesús López-Saucedo
{"title":"Tectonic geomorphology of mountain relief in the northeast of Mexico. Example of the Santa Rosa, Obayos and Pájaros Azules ranges","authors":"Yuri Almaguer-Carmenates, José Alberto Batista-Rodríguez, Ramón Yosvanis Batista-Cruz, Felipe de Jesús López-Saucedo","doi":"10.1016/j.jsames.2025.105513","DOIUrl":null,"url":null,"abstract":"<div><div>A tectonic geomorphology analysis was carried out in the Santa Rosa, Obayos and Pájaros Azules ranges, with the aim of delving deeper into the regional geological characteristics of northeastern Mexico. The digital processing and interpretation of morphometric maps and geomorphic indices derived from a digital elevation model (DEM) at a scale of 1:50,000 was carried out. Hypsometric, surface drainage, slope, roughness, vertical dissection (VD), isobase, channel gradient and mountain-front sinuosity index maps were interpreted. The analysis reveals, in the Obayos and Pájaros Azules ranges, the development of internal valleys with fluvial drainage to the NE, parallel to the axis of the homonymous anticlines. The Santa Rosa range has a higher altitude and gradient than Obayos and Pájaros Azules. According to the 2nd- and 3rd-order isobases, the Santa Rosa range has higher altitudes (1485 m and 1539 m) than Pájaros Azules (1476 m and 878 m) and Obayos (1163 m and 1085 m), respectively. Morphoalignments with NE-SW directions were identified that are arranged transversely to the axes of the anticlines that form the ranges. In the Santa Rosa SE area, the morphoalignments are radial and coincide with basaltic outcrops; this suggests extensional processes due to the flexure of the anticline axis, which generated fissures and caused the ascent of igneous material. The relief in the Obayos and Pájaros Azules ranges is more evolved, due to a greater structural uplift and denudation. In contrast, the Santa Rosa range exhibits a younger relief. The sinuosity index of the mountain front indicates that the three mountain ranges present a moderate level of tectonic activity, with the Obayos mountain range having the lowest Smf value (1.65) and the greatest tectonic activity. These morphotectonic findings show the relationship between regional tectonic evolution and morphogenic processes in NE Mexico.</div></div>","PeriodicalId":50047,"journal":{"name":"Journal of South American Earth Sciences","volume":"160 ","pages":"Article 105513"},"PeriodicalIF":1.7000,"publicationDate":"2025-04-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of South American Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0895981125001750","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
A tectonic geomorphology analysis was carried out in the Santa Rosa, Obayos and Pájaros Azules ranges, with the aim of delving deeper into the regional geological characteristics of northeastern Mexico. The digital processing and interpretation of morphometric maps and geomorphic indices derived from a digital elevation model (DEM) at a scale of 1:50,000 was carried out. Hypsometric, surface drainage, slope, roughness, vertical dissection (VD), isobase, channel gradient and mountain-front sinuosity index maps were interpreted. The analysis reveals, in the Obayos and Pájaros Azules ranges, the development of internal valleys with fluvial drainage to the NE, parallel to the axis of the homonymous anticlines. The Santa Rosa range has a higher altitude and gradient than Obayos and Pájaros Azules. According to the 2nd- and 3rd-order isobases, the Santa Rosa range has higher altitudes (1485 m and 1539 m) than Pájaros Azules (1476 m and 878 m) and Obayos (1163 m and 1085 m), respectively. Morphoalignments with NE-SW directions were identified that are arranged transversely to the axes of the anticlines that form the ranges. In the Santa Rosa SE area, the morphoalignments are radial and coincide with basaltic outcrops; this suggests extensional processes due to the flexure of the anticline axis, which generated fissures and caused the ascent of igneous material. The relief in the Obayos and Pájaros Azules ranges is more evolved, due to a greater structural uplift and denudation. In contrast, the Santa Rosa range exhibits a younger relief. The sinuosity index of the mountain front indicates that the three mountain ranges present a moderate level of tectonic activity, with the Obayos mountain range having the lowest Smf value (1.65) and the greatest tectonic activity. These morphotectonic findings show the relationship between regional tectonic evolution and morphogenic processes in NE Mexico.
期刊介绍:
Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields:
-Economic geology, metallogenesis and hydrocarbon genesis and reservoirs.
-Geophysics, geochemistry, volcanology, igneous and metamorphic petrology.
-Tectonics, neo- and seismotectonics and geodynamic modeling.
-Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research.
-Stratigraphy, sedimentology, structure and basin evolution.
-Paleontology, paleoecology, paleoclimatology and Quaternary geology.
New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.