<?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>S1405-33222021000200009</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2021v73n2a181220</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Análisis paleosísmico de la falla El Malpaso - El Salto, norte de Michoacán, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Paleoseismological analysis of El Malpaso - El Salto fault, north Michoacán, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Soria-Caballero]]></surname>
<given-names><![CDATA[Diana Cinthia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gómez-Calderón]]></surname>
<given-names><![CDATA[Daniel Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[Víctor Hugo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Escuela Nacional de Estudios Superiores ]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Escuela Nacional de Estudios Superiores Posgrado en Ciencias de la Tierra]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Michoacana de San Nicolás de Hidalgo Instituto de Investigaciones en Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>73</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222021000200009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222021000200009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222021000200009&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La falla El Malpaso-El Salto es una estructura con geometría en échelon, compuesta por seis segmentos principales que combinados alcanzan una longitud total de 28 km y que pertenece a la porción occidental del Sistema de Fallas Morelia-Acambay. Esta falla afecta unidades geológicas de edades variables, desde 18 Ma en la zona sur del lago de Cuitzeo hasta 1.5 Ma en la región norte del Complejo Volcánico del Tzirate. La expresión de esta falla en el paisaje y la reciente ocurrencia de sismos de magnitud moderada en la zona indican que puede tener actividad tectónica importante. El análisis paleosísmico preliminar realizado en este trabajo permitió estimar que la falla El Malpaso-El Salto presenta tasas de deslizamiento a largo plazo (slip rate geológico) de 0.086 ± 0.015 mm/año, con períodos de recurrencia de 10021 ± 1221 años, produciendo desplazamientos verticales por evento de entre 80 y 100 cm. De acuerdo a las relaciones empíricas resueltas para esta falla, si sufriera una ruptura en la totalidad de su longitud, tendría la capacidad de producir eventos con magnitudes máximas MW en el rango de 6.6 a 7.3, lo cual es similar a las magnitudes máximas reportadas para otras fallas del Sistema de Fallas Morelia-Acambay. En la zona, la falla El Malpaso-El Salto posee características geométricas, dimensiones, dirección, tipo de movimiento y potencialidad muy similares a las de una falla paralela ubicada a menos de 3 km al sureste y que es conocida como la falla La Alberca-Teremendo. Ambas fallas tienen una orientación favorable respecto al campo de esfuerzos actual (extensión NO-SE) y sus geometrías lístricas sugieren que podrían interaccionar entre ellas durante un evento de ruptura, modificando las estimaciones de recurrencia y magnitud máxima esperada. Las interacciones entre fallas incrementan la peligrosidad del sistema, por lo que su estudio es especialmente importante para las evaluaciones de riesgo sísmico del centro de México. En el sector oeste del Sistema de Fallas Morelia-Acambay son necesarios más estudios para refinar las estimaciones de actividad de las fallas y comprender su comportamiento conjunto.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The El Malpaso - El Salto fault is a structure with en échelon geometry, composed of six main segments which combined has a length of 28 km. This fault belongs to the western sector of the Morelia-Acambay Fault System and affects Miocene - Pleistocene volcanic deposits related to the Cuitzeo ignimbrite and El Tzirate Volcanic Complex (18 and &lt; 1.5 Ma, respectively). The landscape expression of this fault and the recent occurrence of earthquakes of moderate magnitude in the zone indicate that the studied fault could have important tectonic activity. The paleoseismic analysis of this work led us to estimate long-term slip rates (geologic SR) of 0.086 ± 0.015 mm/year and recurrence intervals of 10021 ± 1221 years, considering a total vertical displacement between 80 and 100 cm. According to empirical relationships resolvedfor the MASF, if the fault broke along its entire length, it would have the capacity to produce events with maximum magnitudes (MW) of 6.6 to 7.3, similar to the maximum magnitude reported for other faults in the Morelia- Acambay Fault System. In the study zone, the El Malpaso-El Salto fault has analogous characteristics (such as geometry, dimensions, direction, movement and potentiality) to a neighbor parallel fault named La Alberca-Teremendofault, located3 km southeast of the El Malpaso-El Salto fault trace. Bothfaults are favorably oriented to the current stress field (NW-SE extension) and their listric geometries suggest a probable interaction between them during a rupture event. The interaction with otherfaults of the same system could modify the estimated recurrence interval and maximum expected magnitude; also faults interactions increase the fault's hazard, therefore its study is important for the seismic risk assessment in central México. Also, more detailed studies are necessary to evaluate the activity of the western part of the Morelia Acambay Fault System.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Paleosismología]]></kwd>
<kwd lng="es"><![CDATA[falla El Malpaso-El Salto]]></kwd>
<kwd lng="es"><![CDATA[Sistema de Fallas Morelia-Acambay]]></kwd>
<kwd lng="es"><![CDATA[peligrosidad sísmica]]></kwd>
<kwd lng="en"><![CDATA[Paleoseismology]]></kwd>
<kwd lng="en"><![CDATA[El Malpaso-El Salto fault]]></kwd>
<kwd lng="en"><![CDATA[Morelia-Acambay Fault System]]></kwd>
<kwd lng="en"><![CDATA[seismic hazard]]></kwd>
</kwd-group>
</article-meta>
</front><back>
<ref-list>
<ref id="B1">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Anderson]]></surname>
<given-names><![CDATA[J.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Wesnousky]]></surname>
<given-names><![CDATA[S.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Stirling]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Earthquake size as a function of fault slip rate]]></article-title>
<source><![CDATA[Bulletin of the Seismological Society of America]]></source>
<year>1996</year>
<volume>86</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>683-90</page-range></nlm-citation>
</ref>
<ref id="B2">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Arzate]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Lacan]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Corbo-Camargo]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Arango-Galván]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Felix-Maldonado]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Pacheco]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[León-Loya]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Crustal structure of the eastern Acambay Graben, Central Mexico, from integrated geophysical data]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>2018</year>
<volume>35</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>228-39</page-range></nlm-citation>
</ref>
<ref id="B3">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Avellán]]></surname>
<given-names><![CDATA[D.R.]]></given-names>
</name>
<name>
<surname><![CDATA[Cisneros-Máximo]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Macías]]></surname>
<given-names><![CDATA[J.L.]]></given-names>
</name>
<name>
<surname><![CDATA[Gómez-Vasconcelos]]></surname>
<given-names><![CDATA[M.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Layer]]></surname>
<given-names><![CDATA[P.W.]]></given-names>
</name>
<name>
<surname><![CDATA[Sosa-Ceballos]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Robles-Camacho]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Eruptive chronology of monogenetic volcanoes northwestern of Morelia-Insights into volcano-tectonic interactions in the central-eastern Michoacán-Guanajuato Volcanic Field, México]]></article-title>
<source><![CDATA[Journal of South American Earth Sciences]]></source>
<year>2020</year>
<volume>100</volume>
</nlm-citation>
</ref>
<ref id="B4">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Ego]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Ansan]]></surname>
<given-names><![CDATA[V.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Why is the Central Trans-Mexican Volcanic Belt (102°-99° W) in transtensive deformation?]]></article-title>
<source><![CDATA[Tectonophysics]]></source>
<year>2002</year>
<volume>359</volume>
<page-range>189-208</page-range></nlm-citation>
</ref>
<ref id="B5">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[García-Palomo]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Macías]]></surname>
<given-names><![CDATA[J.L.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Miocene to Recent structural evolution of the Nevado de Toluca volcano region, central Mexico]]></article-title>
<source><![CDATA[Tectonophysics]]></source>
<year>2000</year>
<volume>318</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>281-302</page-range></nlm-citation>
</ref>
<ref id="B6">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[V. H.]]></given-names>
</name>
<name>
<surname><![CDATA[Pérez-López]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Israde-Alcántara]]></surname>
<given-names><![CDATA[I.]]></given-names>
</name>
<name>
<surname><![CDATA[Rodríguez-Pascua]]></surname>
<given-names><![CDATA[M.A.]]></given-names>
</name>
<name>
<surname><![CDATA[Szynkaruk]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Hernández-Madrigal]]></surname>
<given-names><![CDATA[V.M.]]></given-names>
</name>
<name>
<surname><![CDATA[García-Zepeda]]></surname>
<given-names><![CDATA[M.L.]]></given-names>
</name>
<name>
<surname><![CDATA[Corona-Chávez]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Ostroumov]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Medina-Vega]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
<name>
<surname><![CDATA[García-Estrada]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Carranza]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
<name>
<surname><![CDATA[López-Granados]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Mora Chaparro]]></surname>
<given-names><![CDATA[J. C.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Paleoseismology of the southwestern Morelia-Acambay fault system, central Mexico]]></article-title>
<source><![CDATA[Geofísica Internacional]]></source>
<year>2009</year>
<volume>48</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>319-35</page-range></nlm-citation>
</ref>
<ref id="B7">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Gómez-Vasconcelos]]></surname>
<given-names><![CDATA[M.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Macías]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Avellán]]></surname>
<given-names><![CDATA[D.R.]]></given-names>
</name>
<name>
<surname><![CDATA[Sosa-Ceballos]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
<name>
<surname><![CDATA[Cisneros-Máximo]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Layer]]></surname>
<given-names><![CDATA[P.W.]]></given-names>
</name>
<name>
<surname><![CDATA[Benowitz]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[López-Loera]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[López]]></surname>
<given-names><![CDATA[F.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Perton]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[The control of preexisting faults on the distribution, morphology, and volume of monogenetic volcanism in the Michoacán-Guanajuato Volcanic Field]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>2020</year>
<volume>132</volume>
<numero>11-12</numero>
<issue>11-12</issue>
<page-range>2455-74</page-range></nlm-citation>
</ref>
<ref id="B8">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Gómez-Vasconcelos]]></surname>
<given-names><![CDATA[M. G.]]></given-names>
</name>
<name>
<surname><![CDATA[Avellán]]></surname>
<given-names><![CDATA[D. R.]]></given-names>
</name>
<name>
<surname><![CDATA[Soria-Caballero]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Macías]]></surname>
<given-names><![CDATA[J. L.]]></given-names>
</name>
<name>
<surname><![CDATA[Velázquez-Bucio]]></surname>
<given-names><![CDATA[M. M.]]></given-names>
</name>
<name>
<surname><![CDATA[Jiménez-Haro]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Israde-Alcántara]]></surname>
<given-names><![CDATA[I.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[VH.]]></given-names>
</name>
<name>
<surname><![CDATA[Ávila-Olivera]]></surname>
<given-names><![CDATA[J.A.]]></given-names>
</name>
<name>
<surname><![CDATA[Figueroa-Soto]]></surname>
<given-names><![CDATA[A.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Cisneros-Máximo]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Cardona-Melchor]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Geomorphic characterization of faults as earthquake sources in the Cuitzeo Lake basin, central México]]></article-title>
<source><![CDATA[Journal of South American Earth Sciences]]></source>
<year>2021</year>
<volume>109</volume>
</nlm-citation>
</ref>
<ref id="B9">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Iezzi]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Mildon]]></surname>
<given-names><![CDATA[Z.]]></given-names>
</name>
<name>
<surname><![CDATA[Walker]]></surname>
<given-names><![CDATA[J. F.]]></given-names>
</name>
<name>
<surname><![CDATA[Roberts]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Goodall]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[Wilkinson]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Robertson]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Coseismic throw variation across along-strike bends on active normal faults: Implications for displacement versus length scaling of earthquake ruptures]]></article-title>
<source><![CDATA[Journal of Geophysical Research: Solid Earth]]></source>
<year>2018</year>
<volume>123</volume>
<numero>11</numero>
<issue>11</issue>
<page-range>9817-41</page-range></nlm-citation>
</ref>
<ref id="B10">
<nlm-citation citation-type="">
<collab>Instituto Nacional de Estadística y Geografía</collab>
<source><![CDATA[Cartas topográficas 1:50000, Coeneo de la Libertad, Morelia y Patzcuaro]]></source>
<year>2010</year>
</nlm-citation>
</ref>
<ref id="B11">
<nlm-citation citation-type="">
<collab>Instituto Nacional de Estadística y Geografía</collab>
<source><![CDATA[Fotografías aéreas 1:20000, Coeneo de la Libertad]]></source>
<year>2010</year>
</nlm-citation>
</ref>
<ref id="B12">
<nlm-citation citation-type="">
<collab>Instituto Nacional de Estadística y Geografía</collab>
<source><![CDATA[Modelo LIDAR 15 m de resolución, Morelia]]></source>
<year>2010</year>
</nlm-citation>
</ref>
<ref id="B13">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Israde-Alcántara]]></surname>
<given-names><![CDATA[I.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Lacustrine record in a volcanic intra-arc setting. The evolution of the Late Neogene Cuitzeo basin system (Central western Michoacan, Mexico)]]></article-title>
<source><![CDATA[Palaeogeography, Palaeoclimatology, Palaeoecology]]></source>
<year>1999</year>
<volume>151</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>209-27</page-range></nlm-citation>
</ref>
<ref id="B14">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Israde Alcántara]]></surname>
<given-names><![CDATA[I.]]></given-names>
</name>
<name>
<surname><![CDATA[Velázquez-Durán]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Lozano García]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Bischoff]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Domínguez Vázquez]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño Monroy]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Evolución paleolimnológica del Lago Cuitzeo, Michoacán durante el Pleistoceno-Holoceno]]></article-title>
<source><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></source>
<year>2010</year>
<volume>62</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>345-57</page-range></nlm-citation>
</ref>
<ref id="B15">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Kshirsagar]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Siebe]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Guilbaud]]></surname>
<given-names><![CDATA[M. N.]]></given-names>
</name>
<name>
<surname><![CDATA[Salinas]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Layer]]></surname>
<given-names><![CDATA[P W.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Late Pleistocene Alberca de Guadalupe maar volcano (Zacapu basin, Michoacán): Stratigraphy, tectonic setting, and paleo-hydrogeological environment]]></article-title>
<source><![CDATA[Journal of Volcanology and Geothermal Research]]></source>
<year>2015</year>
<volume>304</volume>
<page-range>214-36</page-range></nlm-citation>
</ref>
<ref id="B16">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Lacan]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Ortuño]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Audin]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Perea]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[Baize]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Aguirre-Díaz]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Zúñiga]]></surname>
<given-names><![CDATA[F. R.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Sedimentary evidence of historical and prehistorical earthquakes along the Venta de Bravo Fault System, Acambay Graben (Central Mexico)]]></article-title>
<source><![CDATA[Sedimentary Geology]]></source>
<year>2018</year>
<volume>365</volume>
<page-range>62-77</page-range></nlm-citation>
</ref>
<ref id="B17">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Lafuente Tomás]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
</person-group>
<source><![CDATA[Tectónica activa y paleosismicidad de la falla de Concud (Cordillera Ibérica central)]]></source>
<year>2011</year>
<publisher-name><![CDATA[Universidad de Zaragoza]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B18">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Langridge]]></surname>
<given-names><![CDATA[R.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Weldon II]]></surname>
<given-names><![CDATA[R.J.]]></given-names>
</name>
<name>
<surname><![CDATA[Moya]]></surname>
<given-names><![CDATA[J.C.]]></given-names>
</name>
<name>
<surname><![CDATA[Suárez]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Paleoseismology of the 1912 Acambay earthquake and the Acambay-Tixmadejé Fault, Trans-Mexican Volcanic Belt]]></article-title>
<source><![CDATA[Journal of Geophysical Research, Solid Earth]]></source>
<year>2000</year>
<volume>105</volume>
<numero>B2</numero>
<issue>B2</issue>
<page-range>3019-37</page-range></nlm-citation>
</ref>
<ref id="B19">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Langridge]]></surname>
<given-names><![CDATA[R.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Persaud]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Zúñiga]]></surname>
<given-names><![CDATA[F.R.]]></given-names>
</name>
<name>
<surname><![CDATA[Aguirre-Díaz]]></surname>
<given-names><![CDATA[G.J.]]></given-names>
</name>
<name>
<surname><![CDATA[Villamor]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Lacan]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Preliminary paleoseismic results from the Pastores fault and its role in the seismic hazard of the Acambay graben, Trans-Mexican Volcanic Belt, Mexico]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>2013</year>
<volume>30</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>463-81</page-range></nlm-citation>
</ref>
<ref id="B20">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Martínez-Reyes]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Nieto-Samaniego]]></surname>
<given-names><![CDATA[A.F.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Efectos Geológicos de la Tectónica Reciente en la Parte Central de México]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>1990</year>
<volume>9</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>33-50</page-range></nlm-citation>
</ref>
<ref id="B21">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[McCalpin]]></surname>
<given-names><![CDATA[J.P.]]></given-names>
</name>
</person-group>
<source><![CDATA[Paleoseismology]]></source>
<year>1996</year>
<publisher-loc><![CDATA[San Diego, California ]]></publisher-loc>
<publisher-name><![CDATA[Academic Press]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B22">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Mendoza-Ponce]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Figueroa-Soto]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Soria-Caballero]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[V. H.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Active faults sources for the Pátzcuaro- Acambay fault system (Mexico): fractal analysis of slip rates and magnitudes Mw estimated from fault length]]></article-title>
<source><![CDATA[Natural Hazards &amp; Earth System Sciences]]></source>
<year>2018</year>
<volume>18</volume>
<numero>11</numero>
<issue>11</issue>
<page-range>3121-35</page-range></nlm-citation>
</ref>
<ref id="B23">
<nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Mennella]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
<name>
<surname><![CDATA[Bonassi]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Fault-slip analysis in the basal units of the Mexican Volcanic Belt on the eastern flank of the Tzitzio anticline, Michoacán, México]]></article-title>
<person-group person-group-type="editor">
<name>
<surname><![CDATA[Delgado-Granados]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[Aguirre-Díaz]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Stock]]></surname>
<given-names><![CDATA[J.M.]]></given-names>
</name>
</person-group>
<source><![CDATA[Cenozoic Tectonics and Volcanism of Mexico]]></source>
<year>2000</year>
<volume>334</volume>
<page-range>237-46</page-range><publisher-loc><![CDATA[Boulder, Colorado ]]></publisher-loc>
</nlm-citation>
</ref>
<ref id="B24">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Mennella]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
</person-group>
<source><![CDATA[Sismotectónica del sector occidental del Sistema Morelia-Acambay, México, a partir del análisis de poblaciones de fallas]]></source>
<year>2011</year>
<publisher-name><![CDATA[Universidad Michoacana de San Nicolás de Hidalgo]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B25">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Ortuño]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Zúñiga]]></surname>
<given-names><![CDATA[F. R.]]></given-names>
</name>
<name>
<surname><![CDATA[Aguirre-Díaz]]></surname>
<given-names><![CDATA[G. J.]]></given-names>
</name>
<name>
<surname><![CDATA[Carreón-Freyre]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Cerca]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Roverato]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Holocene paleo-earthquakes recorded at the transfer zone of two major faults: The Pastores and Venta de Bravo faults (Trans-Mexican Volcanic Belt)]]></article-title>
<source><![CDATA[Geosphere]]></source>
<year>2015</year>
<volume>11</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>160-84</page-range></nlm-citation>
</ref>
<ref id="B26">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Ortuño]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Corominas]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
<name>
<surname><![CDATA[Villamor]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Zúñiga]]></surname>
<given-names><![CDATA[R. F.]]></given-names>
</name>
<name>
<surname><![CDATA[Lacan]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Aguirre-Díaz]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Perea]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[&#352;t&#277;pan&#269;íková]]></surname>
<given-names><![CDATA[P]]></given-names>
</name>
<name>
<surname><![CDATA[Ramírez-Herrera]]></surname>
<given-names><![CDATA[M. T.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Evidence of recent ruptures in the central faults of the Acambay Graben (central Mexico)]]></article-title>
<source><![CDATA[Geomorphology]]></source>
<year>2019</year>
<volume>326</volume>
<page-range>17-37</page-range></nlm-citation>
</ref>
<ref id="B27">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Pérez-Orozco]]></surname>
<given-names><![CDATA[J.D.]]></given-names>
</name>
<name>
<surname><![CDATA[Sosa-Ceballos]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
<name>
<surname><![CDATA[Avellán]]></surname>
<given-names><![CDATA[D.R.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Felsic-intermediate magmatism and brittle deformation in Sierra del Tzirate (Michoacán-Guanajuato Volcanic Field)]]></article-title>
<source><![CDATA[Journal of South American Earth Sciences]]></source>
<year>2018</year>
<volume>85</volume>
<page-range>81-96</page-range></nlm-citation>
</ref>
<ref id="B28">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Quigley]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Mohammadi]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[Jiménez]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Duffy]]></surname>
<given-names><![CDATA[B.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Multi-fault earthquakes with kinematic and geometric rupture complexity: how common?]]></article-title>
<source><![CDATA[8th International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology (PATA), 13- 16 November, 2017, New Zealand]]></source>
<year>2017</year>
<page-range>316-8</page-range><publisher-name><![CDATA[INQUA Focus Group Earthquake Geology and Seismic Harzards]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B29">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Quintero-Legorreta]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Análisis estructural de fallas potencialmente activas]]></article-title>
<source><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></source>
<year>2002</year>
<volume>55</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>12-29</page-range></nlm-citation>
</ref>
<ref id="B30">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Rodríguez-Pérez]]></surname>
<given-names><![CDATA[Q.]]></given-names>
</name>
<name>
<surname><![CDATA[Zúñiga]]></surname>
<given-names><![CDATA[F.R.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Seismicity characterization of the Maravatío-Acambay and Actopan regions, central Mexico]]></article-title>
<source><![CDATA[Journal of South American Earth Sciences]]></source>
<year>2017</year>
<volume>76</volume>
<page-range>264-75</page-range></nlm-citation>
</ref>
<ref id="B31">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Singh]]></surname>
<given-names><![CDATA[S.K.]]></given-names>
</name>
<name>
<surname><![CDATA[Iglesias]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño]]></surname>
<given-names><![CDATA[V H.]]></given-names>
</name>
<name>
<surname><![CDATA[Quintanar]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Ordaz]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[A source of the October, 2007 earthquake sequence of Morelia, Mexico and ground-motion estimation from larger earthquakes in the region]]></article-title>
<source><![CDATA[Geofísica Internacional]]></source>
<year>2012</year>
<volume>51</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>73-86</page-range></nlm-citation>
</ref>
<ref id="B32">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Soria-Caballero]]></surname>
<given-names><![CDATA[D.C.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
<name>
<surname><![CDATA[Alcala]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Velázquez-Bucio]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Grassi]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Evidence for quaternary seismic activity of the La Alberca-Teremendo fault, Morelia region, Trans-Mexican Volcanic Belt]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>2019</year>
<volume>36</volume>
<numero>2</numero>
<issue>2</issue>
<page-range>242-58</page-range></nlm-citation>
</ref>
<ref id="B33">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Stirling]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Rhoades]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Berryman]]></surname>
<given-names><![CDATA[K.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Comparison of Earthquake Scaling Relations Derived from Data of the Instrumental and Preinstrumental Era]]></article-title>
<source><![CDATA[Bulletin of the Seismological Society of America]]></source>
<year>2002</year>
<volume>92</volume>
<numero>2</numero>
<issue>2</issue>
<page-range>812-30</page-range></nlm-citation>
</ref>
<ref id="B34">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Sunye-Puchol]]></surname>
<given-names><![CDATA[I.]]></given-names>
</name>
<name>
<surname><![CDATA[Lacan]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Ortuño]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Villamor]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Audin]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Zúñiga]]></surname>
<given-names><![CDATA[F. R.]]></given-names>
</name>
<name>
<surname><![CDATA[Langridge]]></surname>
<given-names><![CDATA[R. M.]]></given-names>
</name>
<name>
<surname><![CDATA[Aguirre-Díaz]]></surname>
<given-names><![CDATA[G. J.]]></given-names>
</name>
<name>
<surname><![CDATA[Lawton]]></surname>
<given-names><![CDATA[T. F.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[La falla San Mateo: nuevas evidencias paleosismológicas de fallamiento activo en el graben de Acambay, México]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>2015</year>
<volume>32</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>361-76</page-range></nlm-citation>
</ref>
<ref id="B35">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Suter]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Quintero-Legorreta]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
<name>
<surname><![CDATA[Johnson]]></surname>
<given-names><![CDATA[C.A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Active faults and state of stress in the central part of the Trans-Mexican Volcanic Belt, Mexico; 1, The Venta de Bravo Fault]]></article-title>
<source><![CDATA[Journal of Geophysical Research]]></source>
<year>1992</year>
<volume>97</volume>
<page-range>11983-93</page-range></nlm-citation>
</ref>
<ref id="B36">
<nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Suter]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<source><![CDATA[Active Faults in the central part of the Trans-Mexican Volcanic Belt, Mexico. Compilation for the map of major active faults, western Hemisphere, International Lithosphere Program (ILP), Project II-2. December 1994, updated 2002]]></source>
<year>2002</year>
</nlm-citation>
</ref>
<ref id="B37">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Suter]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[López-Martínez]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Quintero-Legorreta]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
<name>
<surname><![CDATA[Carrillo-Martínez]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Quaternary intra-arc extension in the Central Trans-Mexican volcanic belt]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>2001</year>
<volume>113</volume>
<numero>6</numero>
<issue>6</issue>
<page-range>693-703</page-range></nlm-citation>
</ref>
<ref id="B38">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Suter]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[The AD 1567 Mw 7.2 Ameca, Jalisco, Earthquake (Western Trans-Mexican Volcanic Belt): Surface Rupture Parameters, Seismogeological Effects, and Macroseismic Intensities from Historical Sources]]></article-title>
<source><![CDATA[Bulletin of the Seismological Society of America]]></source>
<year>2015</year>
<volume>105</volume>
<numero>2A</numero>
<issue>2A</issue>
<page-range>646-56</page-range></nlm-citation>
</ref>
<ref id="B39">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Suter]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Structure and Holocene rupture of the Morelia fault, Trans-Mexican volcanic belt, and their significance for seismic-hazard assessment]]></article-title>
<source><![CDATA[Bulletin of the Seismological Society of America]]></source>
<year>2016</year>
<volume>106</volume>
<numero>5</numero>
<issue>5</issue>
<page-range>2376-88</page-range></nlm-citation>
</ref>
<ref id="B40">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Urbina]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Camacho]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[La zona megasísmica Acambay- Tixmadejé, Estado de México, conmovida el 19 de noviembre de 1912]]></article-title>
<source><![CDATA[Boletín del Instituto Geológico de México]]></source>
<year>1913</year>
<volume>32</volume>
</nlm-citation>
</ref>
<ref id="B41">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Velázquez-Bucio]]></surname>
<given-names><![CDATA[M.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[V.H.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Soft-sediment deformation structures induced by seismic activity in the San Pedro el Alto area, Acambay graben, México]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>2018</year>
<volume>35</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>28-40</page-range></nlm-citation>
</ref>
<ref id="B42">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Wells]]></surname>
<given-names><![CDATA[D.L.]]></given-names>
</name>
<name>
<surname><![CDATA[Coppersmith]]></surname>
<given-names><![CDATA[K.J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement]]></article-title>
<source><![CDATA[Bulletin of the Seismological Society of America]]></source>
<year>1994</year>
<volume>84</volume>
<page-range>974-1002</page-range></nlm-citation>
</ref>
<ref id="B43">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Wesnousky]]></surname>
<given-names><![CDATA[S.G.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Displacement and geometrical characteristics of earthquake surface ruptures: Issues and implications for seismic-hazard analysis and the process of earthquake rupture]]></article-title>
<source><![CDATA[Bulletin of the Seismological Society of America]]></source>
<year>2008</year>
<volume>98</volume>
<numero>4</numero>
<issue>4</issue>
<page-range>1609-32</page-range></nlm-citation>
</ref>
</ref-list>
</back>
</article>
