<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222024000200105</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2024v76n2a020324</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Identificación de la respuesta sísmica en pirámides del área de Chichén Itzá para preservar el patrimonio cultural]]></article-title>
<article-title xml:lang="en"><![CDATA[Identification of the seismic response in pyramids of the Chichén Itzá area for the preservation of cultural heritage]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cárdenas-Soto]]></surname>
<given-names><![CDATA[Martín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-González]]></surname>
<given-names><![CDATA[Jesús]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martínez-González]]></surname>
<given-names><![CDATA[José A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Escobedo-Zenil]]></surname>
<given-names><![CDATA[David]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sandoval-Quintana]]></surname>
<given-names><![CDATA[Osiris]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carrillo-Vargas]]></surname>
<given-names><![CDATA[Armando]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Argote-Espino]]></surname>
<given-names><![CDATA[Denisse L.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López-Garcia]]></surname>
<given-names><![CDATA[Pedro A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cifuentes-Nava]]></surname>
<given-names><![CDATA[Gerardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Facultad de Ingeniería Departamento de Geofísica, División de Ingeniería en Ciencias de la Tierra]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Servicio Magnético]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Instituto Nacional de Antropología e Historia Dirección de Estudios Arqueológicos ]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Escuela Nacional de Antropología e Historia Posgrado en Arqueología ]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<volume>76</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222024000200105&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222024000200105&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222024000200105&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Analizamos la respuesta sísmica de tres estructuras arqueológicas de la zona Chichén Itzá a fin de proveer elementos que permitan dar seguimiento a su preservación. Realizamos medidas de ruido sísmico ambiental con sismógrafos triaxiales de banda ancha por un periodo de tres días para cuantificar las frecuencias de vibración de los edificios de Las Monjas, El Caracol, y El Castillo o Pirámide de Kukulkán mediante cocientes espectrales HVSR. Los resultados muestran que en El Caracol predomina la frecuencia del suelo en 1.3 Hz. Sin embargo, en los edificios Las Monjas y El Castillo observamos una frecuencia fundamental de vibrar de 5.1 Hz con una amplificación relativa alrededor de 6. Este resultado muestra que estas dos pirámides se comportan como una capa de suelo sobre un estrato rígido. En el caso de El Castillo, el registro de ruido en un sismógrafo en su base permite observar un efecto de interacción cinemática debido a la diferencia de rigidez entre el suelo y la estructura. No observamos algún efecto direccional en los cocientes HVSR debido a la anisotropía interna de las pirámides. La estimación de la velocidad de corte es de 255 m/s (considerando que la respuesta sísmica es de origen topográfico, es decir, debido a que la pirámide representa una irregularidad en la superficie del suelo). Esta velocidad corresponde a materiales poco compactos que descansan sobre calizas competentes con velocidad mayores a 1000 m/s, materiales que son susceptibles a sufrir cambios de esfuerzos que eventualmente puede llevar a un deterioro estructural. Los hallazgos de este estudio sugieren que es necesario un seguimiento e instrumentación continua de los niveles inferiores para evaluar la influencia de las subestructuras durante las etapas preconstructivas y determinar si existen otros efectos debido a la naturaleza kárstica del subsuelo.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In this study, an analysis was conducted on the seismic response of three archaeological structures located in the Chichén Itzá area. The objective of this analysis was to gather relevant information that may be utilized to monitor and ensure the preservation of these monuments. Ambient seismic noise measurements were conducted over three days using broad-band seismographs. The objective was to assess the vibration frequencies of three buildings, namely Las Monjas, El Caracol and El Castillo or Kukulkan Pyramid, using HVSR method. The findings indicate that the dominant frequency of the El Caracol building is 1.3 Hz. Nevertheless, it is noteworthy that within the Las Monjas and El Castillo structures, an observable fundamental frequency of 5.1 Hz is present, accompanied by a relative amplification of around 6. The findings of this study indicate the behavior of the two pyramids can be likened to that of a soil layer overlaying a stiff stratum. The noise recorded by a seismograph at the base of El Castillo enables the observation of a kinematic interaction phenomenon resulting from the disparate stiffness properties of the soil and the structure. No directional effect was observed on the HVSR ratios due to internal irregularities in the pyramids. Considering the half-width of the base of each pyramid and that the site response is of topographic origin, the calculus of shear velocity is 255 m/s. This velocity relates to non-compact materials resting on competent rocks with velocities more than 1000 m/s, materials subject to stress changes that may eventually lead to structural degradation. The findings of this study indicate the need for continuous monitoring and instrumentation of lower levels to assess the influence of substructures during preconstruction stages and determine whether there are any other effects due to the karstic nature of the subsurface.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[ruido sísmico]]></kwd>
<kwd lng="es"><![CDATA[HVSR]]></kwd>
<kwd lng="es"><![CDATA[interferometría sísmica]]></kwd>
<kwd lng="es"><![CDATA[efectos de sitio topográficos]]></kwd>
<kwd lng="es"><![CDATA[pirámide de Kukulkán]]></kwd>
<kwd lng="en"><![CDATA[seismic noise]]></kwd>
<kwd lng="en"><![CDATA[seismic interferometry]]></kwd>
<kwd lng="en"><![CDATA[HVSR]]></kwd>
<kwd lng="en"><![CDATA[topographic site effects]]></kwd>
<kwd lng="en"><![CDATA[Kukulkan Pyramid]]></kwd>
</kwd-group>
</article-meta>
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