<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692025000401815</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2025.64.4.1859</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Adquisición de datos gravimétricos con Corrección Urbana en la Cuenca de México. Elaboración de carta de anomalía de Bouguer y su análisis cualitativo preliminar]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pita de la Paz]]></surname>
<given-names><![CDATA[Carlos]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Huante Arana]]></surname>
<given-names><![CDATA[Francisco E.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rubio Ramos]]></surname>
<given-names><![CDATA[Marco A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Colchado Casas]]></surname>
<given-names><![CDATA[Juan C.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortiz Ruiz]]></surname>
<given-names><![CDATA[Maricela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Geotem Ingeniería  ]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2025</year>
</pub-date>
<volume>64</volume>
<numero>4</numero>
<fpage>1815</fpage>
<lpage>1832</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692025000401815&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692025000401815&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692025000401815&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Metropolitan Area of Mexico City (MAMC), hosting more than 25 million inhabitants, is located on the south-western side of the Basin of Mexico, a sink (2,200 m.a.s.l.) bordered (confined) cardinally by the four volcanic mountain ranges (3,400, 3,800, 3,900 and 3,000 m.a.s.l.; Las Cruces, Nevada, Chichinautzin and Guadalupe, respectively). This tectonic sink (2,200 m.a.s.l.) is part of the central-eastern sector of the Trans-Mexican Volcanic Belt, whose effusive products cover the southern sector of the Mexican Highlands Plateau on the eastern border of the Guerrero Terrain. The urbanization in the MAMC is exposed to a series of geological risks, particularly those derived from seismicity and soil-structure interaction. Subsurface structural architecture of the basin determines the lateral and vertical distribution of the lithological fill units. This arrangement directly governs the mechanical behavior of the subsoil, influencing the soil-structure interaction of the buildings constructed on the surface units. From the seismic record is well documented that the main urban damage and spatial distribution risk occurred near the borders of several depocenters and/or closer to surficial inferred structural lineaments. To characterize the deep geology, a gravity survey was undertook in the MAMC with 2,048 ground stations and three fixed base stations, with a data acquisition spacing between 1 and 3 km in most of the metropolitan area. In areas of greater interest and dense urban infrastructure, more detailed sampling was applied with separations of 100 to 200 m. To improve the reliability of gravity interpretation in Mexico City, an urban gravimetric correction was implemented, allowing for a reduction in the anomalous effects of the infrastructure on the acquired data. The results obtained allows the delineation of anomaly limits and deep structures totally or partially hidden under the sedimentary units. These results constitute a basis for the evaluation of geological risk and the planning of mitigation strategies in the region.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La Zona Metropolitana de la Ciudad de México (ZMCM), con una población superior a los 25 millones de habitantes, se ubica en el sector suroccidental de la Cuenca de México (CM). Esta cuenca está bordeada (confinada) cardinalmente por cuatro sierras volcánicas (3,400, 3,800, 3,900 y 3,000 m.s.n.m.; Las Cruces, Nevada, Chichinautzin y Guadalupe, respectivamente). Esta depresión tectónica (2,200 m.s.n.m.) forma parte del sector centro-oriental de la Franja Volcánica Trans-Mexicana, cuyos productos efusivos cubren el sector meridional del Altiplano Mexicano en la frontera oriental del Terreno Guerrero. El desarrollo urbano en la ZMCM está expuesto a una serie de riesgos geológicos, particularmente los derivados de la sismicidad y la interacción suelo-estructura. La configuración estructural profunda de la cuenca determina la distribución lateral y vertical de las unidades litológicas de relleno. Esta disposición gobierna directamente el comportamiento mecánico del subsuelo, condicionando la interacción suelo-estructura de las edificaciones construidas sobre las unidades superficiales. En particular, los mayores daños urbanos y la mayor exposición al riesgo sísmico se correlacionan espacialmente con los bordes de los depocentros y su cercanía a lineamientos estructurales superficiales. Para caracterizar la geología profunda en la mayor parte de la ZMCM, desde los materiales de relleno de la CM hasta el zócalo calcáreo o metamórfico en que sobreyacen a 2 o 3 km de profundidad, se realizó un estudio gravimétrico en la cuenca que incluyó 2,048 estaciones terrestres y tres estaciones de base fijas, con un espaciamiento de adquisición de datos entre 1 y 3 km. En zonas de mayor interés y densa infraestructura urbana, se aplicó un muestreo más detallado con separaciones de 100 a 200 m. Para mejorar la confiabilidad de la interpretación gravimétrica en la Ciudad de México, se implementó una corrección gravimétrica urbana, permitiendo una reducción en los efectos anómalos de la infraestructura sobre los datos adquiridos. Los resultados obtenidos permitieron delinear límites de anomalías gravimétricas y estructuras profundas total o parcialmente ocultas bajo las unidades volcánicas y vulcanosedimentarias superficiales. Estos resultados constituyen una base fundamental para la evaluación del riesgo geológico y la planificación de estrategias de mitigación en la región.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Urban Gravity Survey]]></kwd>
<kwd lng="en"><![CDATA[Building Correction]]></kwd>
<kwd lng="en"><![CDATA[Basin of Mexico]]></kwd>
<kwd lng="en"><![CDATA[Bouguer Anomaly]]></kwd>
<kwd lng="en"><![CDATA[Mexico City Metropolitan Area]]></kwd>
<kwd lng="es"><![CDATA[Gravimetría urbana]]></kwd>
<kwd lng="es"><![CDATA[Corrección por edificios]]></kwd>
<kwd lng="es"><![CDATA[Cuenca de México]]></kwd>
<kwd lng="es"><![CDATA[Anomalía de Bouguer]]></kwd>
<kwd lng="es"><![CDATA[Zona Metropolitana de la Ciudad de México]]></kwd>
</kwd-group>
</article-meta>
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