<?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>S1405-33222022000100110</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2022v74n1a130821</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Extensión sinsedimentaria del Cretácico Inferior en el borde del Bloque Coahuila, un margen tipo rift en México]]></article-title>
<article-title xml:lang="en"><![CDATA[Lower Cretaceous synsedimentary extension at the edge of the Coahuila Block, a rift-like margin in Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Eguiluz y de Antuñano]]></surname>
<given-names><![CDATA[Samuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Chávez]]></surname>
<given-names><![CDATA[Gabriel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,CDMX  ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Nuevo León Facultad de Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Linares N. L.]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>74</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222022000100110&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222022000100110&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222022000100110&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Este trabajo presenta datos que caracterizan a un sistema de fallas normales lístricas en dominó, con arreglos sintético y antitético en el borde de lo que se presume es una cuenca tipo rift en el noreste de México. Los afloramientos se localizan dentro de las estructuras anticlinales La Gavia y Arteaga, en el Estado de Coahuila y paleogeográficamente en el borde oriental del Bloque de Coahuila. El análisis de tensores de paleoesfuerzos de estas fallas permite definir un vector de extensión &#963;3 perpendicular al borde del Bloque de Coahuila, en La Gavia dirigido ~0°/191°-193° y en Arteaga con dirección de &#963;3 ~0°/200°. Deformación en sedimentos suaves &#8220;no litificados&#8221; también está presente en la sucesión. El análisis estructural de las fallas y las estructuras sedimentarias en sedimentos suaves sugieren que estas deformaciones fueron sincrónicas al relleno de la cuenca y co-genéticas. Este sistema de fallas se restringe a un nivel estratigráfico específico, por lo que se sugiere que tiene un desarrollo contemporáneo con la sedimentación clástica de la Arcosa Patula y la Formación Carbonera durante el Cretácico Inferior. Se interpreta que la extensión que generó estas fallas y la deformación de sedimentos suave puede ser atribuida a diferentes causas: 1) Como consecuencia de esfuerzos tectónicos regionales durante extensión en un ambiente tipo rift, similar en las cuencas de Sabinas y del Centro de México; 2) A una pendiente acentuada de la cuña sedimentaria entre el Bloque de Coahuila y las cuencas durante rejuvenecimiento del relieve, o bien, 3) La combinación de los mecanismos enunciados.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT This work presents data that identify a system of normal lystric domino faults, with synthetic and antithetical arrangements, at the edge of what is presumed to be a rift-type basin in northeastern Mexico. The outcrops are located within La Gavia and Arteaga anticlines, in the State of Coahuila and these localities are located paleogeographically on the eastern edge of the Coahuila Block. The structural analysis of these faults allows defining an extension vector &#963;3 perpendicular to the edge of the Coahuila Block, trending ~ 0 ° /191°-193 ° in La Gavia, and &#963;3 ~ 0 °/ 200° in Arteaga. Deformation in soft &#8220;non-lithified&#8221; sediments is also present in the succession. The structural analysis of the faults and the sedimentary structures in soft sediments suggest that these deformations were synchronous to basin infilling and co-genetics. This fault system is restricted to a specific stratigraphic level; thus, it is suggested that it has a contemporary development with the clastic sedimentation of the Arcosa Patula and the Carbonera Formation during the Lower Cretaceous. It is interpreted that the extension that generated these faults and soft sediment deformation can be attributed to different causes: 1) as a consequence of regional tectonic stress during extension in rift-type environments such as those generated by the Sabinas and Central Mexico basins; 2) a steep slope of the sedimentary wedge between the Coahuila Block and the basins during rejuvenation of the relief, or, 3) the combination of both mechanisms.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[rift]]></kwd>
<kwd lng="es"><![CDATA[fallas sin-sedimentarias]]></kwd>
<kwd lng="es"><![CDATA[slump]]></kwd>
<kwd lng="es"><![CDATA[Arcosa Patula]]></kwd>
<kwd lng="es"><![CDATA[Formación Carbonera]]></kwd>
<kwd lng="en"><![CDATA[rift]]></kwd>
<kwd lng="en"><![CDATA[sin-sedimentary faults]]></kwd>
<kwd lng="en"><![CDATA[slump]]></kwd>
<kwd lng="en"><![CDATA[Patula Arkose]]></kwd>
<kwd lng="en"><![CDATA[Carbonera Formation]]></kwd>
</kwd-group>
</article-meta>
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