<?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>S1405-33222020000100102</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2020v72n1a031019</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Estimación de desplazamiento mínimo en fallas inversas de alto ángulo: Caso de estudio en la Falla de San Marcos, Coahuila]]></article-title>
<article-title xml:lang="en"><![CDATA[Minimum displacement estimation in high-angle reverse faults:Case study in the San Marcos Fault, Coahuila]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alonso-Manuel]]></surname>
<given-names><![CDATA[Fausto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fitz-Díaz]]></surname>
<given-names><![CDATA[Elisa]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gutiérrez-Navarro]]></surname>
<given-names><![CDATA[Rodrigo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>72</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222020000100102&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222020000100102&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222020000100102&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La Falla de San Marcos (FSM) es una estructura que atraviesa al estado de Coahuila con rumbo general NW-SE. Esta estructura forma parte de un sistema de fallas normales en el Jurásico Medio con una reactivación en el Jurásico Tardío, condicionó el depósito de unidades carbonatadas durante el Cretácico Temprano y se reactivó como falla inversa posiblemente en el Paleógeno. El límite nororiental de la plataforma de Coahuila coincide con la traza de la FSM y en la localidad de Las Palomas, Coahuila, es donde mejor se expone. En este sitio las capas de la Formación Cupido cabalgan sobre lutitas calcáreas pelágicas, a las cuales nos referimos informalmente como Capas Cerro La Bruja (CCLB). Esta unidad se correlaciona con la Formación Eagle Ford en la cuenca de Sabinas al norte y con la Formación Indidura en la cuenca de Parras, al sur. Las CCLB se observan sub-horizontales sobre la plataforma de Coahuila, ya que sólo se acortaron en los 400 metros más próximos a la traza de la FSM. La actividad de la falla provocó el desarrollo de pliegues tipo chevron, los cuales se disponen en una cuña de deformación limitada por una falla basal que separa a las rocas plegadas de aquellas no plegadas. Un análisis detallado de pliegues permitió estimar un acortamiento horizontal de alrededor de 500 metros. Considerando que sólo hay una generación de pliegues en las CCLB y que el acortamiento fue causado por la actividad de la FSM. Basado en la estimación de este acortamiento, se propone un nuevo método para estimar el desplazamiento mínimo de la traza frontal del sistema de la FSM, el cual toma en cuenta el acortamiento de las CCLB y la inclinación de la falla. Dicho método permitió estimar un desplazamiento mínimo de 1300 m sobre el plano frontal de la falla, lo cual es consistente con las estimaciones de más de 3000 m, realizadas por autores previos para todo el sistema de fallas. La estimación de desplaza- miento a lo largo de fallas mayores siempre ha sido un reto en el análisis estructural, por lo cual consideramos que nuestro nuevo método puede ser una valiosa herramienta para determinar desplazamiento sobre fallas mayores.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The San Marcos fault (SMF) cuts across Coahuila state along a NW-SE trend. This long-lived structure is part of a Middle Jurassic normal fault system, with a Late Jurassic reactivation, which constrained the deposition of Early Cretaceous red beds and carbonate deposits and was reactivated as reverse fault during Paleogene. The SMF coincides with the northwestern boundary of the Coahuila platform, with its best exposure at Las Palomas village. The Cupido Formation thrust over pelagic limestone, in a locality which was studied in detail and informally referred as Cerro La Bruja beds (CCLB). This unit correlates with the Eagle Ford Formation (EFF) in the Sabinas Basin to the north and with the Indidura Formation in the Parras Basin, to the south, all of Turonian age. The CCLB are involved in kilometer scale folding in both basins. However, these rocks are sub-horizontal in the Coahuila platform, where they were shortened only 400 m in the closest position to the SMF, showing chevron folds within a deformation wedge limited by a basal fault separating folded rocks from unfolded rocks underneath. Near the fault plane and along the thicker portion of the wedge, folds are tighter compared to the furthermost portion. Based on a detailed fold shortening analysis in the CCLB, a horizontal shortening of about 500 meters was estimated for these beds. If we assume that only one folding generation is present in the CCLB and that this shortening event was the result of the SMF activity, we propose a new method to estimate the minimum displacement on the frontal fault, which considers folds of CCLB and the fault plane incli- nation. A minimum displacement of 1300 m is calculated along the fault plane, showing consistency with estimations of at least 3000 m suggested by previous authors for the entire fault system. Fault displacement estimates have always been a challenge in structural analysis, and that is the reason why we consider that our new method has potential to become a valuable tool in fault kinematic analysis.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Desplazamiento falla inversa]]></kwd>
<kwd lng="es"><![CDATA[pliegues chevron]]></kwd>
<kwd lng="es"><![CDATA[falla de San Marcos]]></kwd>
<kwd lng="es"><![CDATA[Capas Cerro la Bruja]]></kwd>
<kwd lng="en"><![CDATA[Thrust fault displacement]]></kwd>
<kwd lng="en"><![CDATA[chevron folds]]></kwd>
<kwd lng="en"><![CDATA[San Marcos fault]]></kwd>
<kwd lng="en"><![CDATA[Capas Cerro La Bruja]]></kwd>
</kwd-group>
</article-meta>
</front><back>
<ref-list>
<ref id="B1">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Alonso-Manuel]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
</person-group>
<source><![CDATA[Estratigrafía y deformación de las Capas Cerro la Bruja, cerca de la Falla de San Marcos, Las Palomas, Coahuila]]></source>
<year>2016</year>
<page-range>110</page-range><publisher-name><![CDATA[Facultad de Ingeniería, Universidad Nacional Autónoma de México]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B2">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Armstrong]]></surname>
<given-names><![CDATA[R.L.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Sevier orogenic belt in Nevada and Utah]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>1968</year>
<volume>79</volume>
<numero>4</numero>
<issue>4</issue>
<page-range>429-58</page-range></nlm-citation>
</ref>
<ref id="B3">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Bergen]]></surname>
<given-names><![CDATA[K.]]></given-names>
</name>
<name>
<surname><![CDATA[Shaw]]></surname>
<given-names><![CDATA[J.H.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Displacement profiles and displacement-length scaling relationships of thrust faults constrained by seismic reflection data]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>2010</year>
<volume>122</volume>
<numero>7-8</numero>
<issue>7-8</issue>
<page-range>1209-19</page-range></nlm-citation>
</ref>
<ref id="B4">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Bolaños-Rodríguez]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
</person-group>
<source><![CDATA[Análisis estructural en el puerto de las sierras la Fragua, El Granizo, San Marcos-Pinos y áreas aledañas en la parte central de Coahuila]]></source>
<year>2006</year>
<publisher-loc><![CDATA[Ciudad de México, México ]]></publisher-loc>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B5">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Campa-Uranga]]></surname>
<given-names><![CDATA[M.F.]]></given-names>
</name>
<name>
<surname><![CDATA[Coney]]></surname>
<given-names><![CDATA[P. J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Tectono-stratigraphic terranes and mineral resource distributions in Mexico]]></article-title>
<source><![CDATA[Canadian Journal of Earth Sciences]]></source>
<year>1983</year>
<volume>20</volume>
<numero>6</numero>
<issue>6</issue>
<page-range>1040-51</page-range></nlm-citation>
</ref>
<ref id="B6">
<nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Campa-Uranga]]></surname>
<given-names><![CDATA[M.F.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[The Mexican thrust belt. Tectonostratigraphic terranes of the circum-Pacific region]]></article-title>
<person-group person-group-type="editor">
<name>
<surname><![CDATA[Howell]]></surname>
<given-names><![CDATA[D.G.]]></given-names>
</name>
</person-group>
<source><![CDATA[Circum-Pacific Council for Energy and Mineral Resources, Houston, Texas: Earth Science Series]]></source>
<year>1985</year>
<volume>1</volume>
<page-range>299-313</page-range></nlm-citation>
</ref>
<ref id="B7">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Carrillo-Martínez]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Geometría estructural de la Sierra Madre Oriental, entre Peñamiller y Jalpan, Estado de Querétaro]]></article-title>
<source><![CDATA[Revista Mexicana Ciencias Geológicas]]></source>
<year>1990</year>
<volume>9</volume>
<page-range>62-70</page-range></nlm-citation>
</ref>
<ref id="B8">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Charleston]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[A summary of the structural geology and tectonicsof the state of Coahuila, Mexico]]></article-title>
<person-group person-group-type="editor">
<name>
<surname><![CDATA[Schmidt]]></surname>
<given-names><![CDATA[C.I.]]></given-names>
</name>
<name>
<surname><![CDATA[Katz]]></surname>
<given-names><![CDATA[S.B.]]></given-names>
</name>
</person-group>
<source><![CDATA[Lower Cretaceous stratigraphy and structure, northern Mexico]]></source>
<year>1981</year>
<page-range>28-36</page-range><publisher-name><![CDATA[West Texas Geological Society, Field Trip Guidebook, Publication]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B9">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Chávez-Cabello]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Aranda-Gómez]]></surname>
<given-names><![CDATA[J.J.]]></given-names>
</name>
<name>
<surname><![CDATA[Molina- Garza]]></surname>
<given-names><![CDATA[R.S.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[La falla San Marcos: una estructura jurásica de basamento multirreactivada del noreste de México]]></article-title>
<source><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></source>
<year>2005</year>
<volume>57</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>27-52</page-range></nlm-citation>
</ref>
<ref id="B10">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Dahlstrom]]></surname>
<given-names><![CDATA[C.D.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Structural geology in the eastern margin of the Canadian Rocky Mountains]]></article-title>
<source><![CDATA[Bulletin of Canadian Petroleum Geology]]></source>
<year>1970</year>
<volume>18</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>332-406</page-range></nlm-citation>
</ref>
<ref id="B11">
<nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Duque-Botero]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Maurrasse]]></surname>
<given-names><![CDATA[F.J.-M.R.]]></given-names>
</name>
<name>
<surname><![CDATA[Hickey- Vargas]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Melinte]]></surname>
<given-names><![CDATA[M.C.]]></given-names>
</name>
<name>
<surname><![CDATA[Jaffe]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[López-Oliva]]></surname>
<given-names><![CDATA[J.G.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Microspherroid Accumulations and Geochemical Characteristics of a Cenomanian-Turonian Anoxic Basin: The Record of the Indidura Formation, NE Mexico]]></article-title>
<person-group person-group-type="editor">
<name>
<surname><![CDATA[Demchuk]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Gary]]></surname>
<given-names><![CDATA[A.C.]]></given-names>
</name>
</person-group>
<source><![CDATA[Geologic Problem Solving with Microfossils: A Volume in Honor of Garry D. Jones]]></source>
<year>2008</year>
<page-range>1-16</page-range></nlm-citation>
</ref>
<ref id="B12">
<nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Eguiluz de Antuñano]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Geologic Evolution and Gas Resources of the Sabinas Basin in Northeastern Mexico]]></article-title>
<person-group person-group-type="editor">
<name>
<surname><![CDATA[Bartolini]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Buffler]]></surname>
<given-names><![CDATA[R.T.]]></given-names>
</name>
<name>
<surname><![CDATA[Cantú-Chapa]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<source><![CDATA[The Western Gulf of Mexico Basin: Tectonics, sedimentary basins, and petroleum systems]]></source>
<year>2001</year>
<page-range>241-70</page-range></nlm-citation>
</ref>
<ref id="B13">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Eguiluz de Antuñano]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Aranda-Garcia]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Marrett]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Tectónica de la Sierra Madre Oriental, México]]></article-title>
<source><![CDATA[Boletín Sociedad Geológica Mexicana]]></source>
<year>2000</year>
<volume>53</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>1-26</page-range></nlm-citation>
</ref>
<ref id="B14">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Fitz-Díaz]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Hudleston]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Tolson]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Comparison of tectonic styles in the Mexican and Canadian Rocky Mountain Fold-Thrust Belt]]></article-title>
<source><![CDATA[The Geological Society of London, Special Publications]]></source>
<year>2011</year>
<volume>349</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>149-67</page-range></nlm-citation>
</ref>
<ref id="B15">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Fitz-Díaz]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Tolson G.]]></surname>
<given-names><![CDATA[Hudleston P.]]></given-names>
</name>
<name>
<surname><![CDATA[Bolaños- Rodríguez]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Ortega-Flores]]></surname>
<given-names><![CDATA[B.]]></given-names>
</name>
<name>
<surname><![CDATA[Vázquez- Serrano]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[The role of folding in the development of the Mexican fold-and-thrust belt]]></article-title>
<source><![CDATA[Geosphere]]></source>
<year>2012</year>
<volume>8</volume>
<numero>4</numero>
<issue>4</issue>
<page-range>931-49</page-range></nlm-citation>
</ref>
<ref id="B16">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Fitz-Díaz]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Hall]]></surname>
<given-names><![CDATA[C.M.]]></given-names>
</name>
<name>
<surname><![CDATA[van der Plujim]]></surname>
<given-names><![CDATA[B.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[XRD-based 40Ar/39Ar age correction for fine-grained illite, with application to folded carbonates in the Monterrey Salient (northern Mexico)]]></article-title>
<source><![CDATA[Geochimica et Cosmochimica Acta]]></source>
<year>2016</year>
<numero>181</numero>
<issue>181</issue>
<page-range>201-16</page-range></nlm-citation>
</ref>
<ref id="B17">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Fitz-Díaz]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Lawton]]></surname>
<given-names><![CDATA[T.F.]]></given-names>
</name>
<name>
<surname><![CDATA[Juárez-Arriaga]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Chávez-Cabello]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[The Cretaceous- Paleogene Mexican orogen: Structure, basin development, magmatism and tectonics]]></article-title>
<source><![CDATA[Earth-Science Reviews]]></source>
<year>2017</year>
<numero>183</numero>
<issue>183</issue>
<page-range>56-84</page-range></nlm-citation>
</ref>
<ref id="B18">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Goldhammer]]></surname>
<given-names><![CDATA[R.K.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Mesozoic sequence stratigraphy and paleogeographic evolution of northeast Mexico]]></article-title>
<source><![CDATA[Geological Society of America]]></source>
<year>1999</year>
<numero>340</numero>
<issue>340</issue>
<page-range>1-58</page-range></nlm-citation>
</ref>
<ref id="B19">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Gray]]></surname>
<given-names><![CDATA[G.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Pottorf]]></surname>
<given-names><![CDATA[R.J.]]></given-names>
</name>
<name>
<surname><![CDATA[Yurewicz]]></surname>
<given-names><![CDATA[D.A.]]></given-names>
</name>
<name>
<surname><![CDATA[Mahon]]></surname>
<given-names><![CDATA[K.I.]]></given-names>
</name>
<name>
<surname><![CDATA[Pevear]]></surname>
<given-names><![CDATA[D.R.]]></given-names>
</name>
<name>
<surname><![CDATA[Chuchla]]></surname>
<given-names><![CDATA[R.J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Thermal and chronological record of synto post-Laramide burial and exhumation, Sierra Madre Oriental, Mexico]]></article-title>
<person-group person-group-type="editor">
<name>
<surname><![CDATA[Bartolini]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Buffler]]></surname>
<given-names><![CDATA[R.T.]]></given-names>
</name>
<name>
<surname><![CDATA[Cantú-Chapa]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<source><![CDATA[The Western Gulf of México Basin, Tectonics, Sedimentary Basins, and Petroleum Systems]]></source>
<year>2001</year>
<volume>75</volume>
<page-range>159-81</page-range><publisher-name><![CDATA[American Association of Petroleum Geologists]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B20">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Gray]]></surname>
<given-names><![CDATA[G.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Lawton]]></surname>
<given-names><![CDATA[T.F.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[New constraints on timing of Hidalgoan (Laramide) deformation in the Parras and La Popa basins, NE Mexico]]></article-title>
<source><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></source>
<year>2011</year>
<volume>63</volume>
<numero>2</numero>
<issue>2</issue>
<page-range>333-43</page-range></nlm-citation>
</ref>
<ref id="B21">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Haenggi]]></surname>
<given-names><![CDATA[W.T.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Tectonic history of the Chihuahua trough, Mexico and adjacent USA, part II: Mesozoic and Cenozoic]]></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>38-94</page-range></nlm-citation>
</ref>
<ref id="B22">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Harbor]]></surname>
<given-names><![CDATA[R.L.]]></given-names>
</name>
</person-group>
<source><![CDATA[Facies Characterization and Stratigraphic Architecture of Organic-Rich Mudrocks, Upper Cretaceous Eagle Ford Formation, South Texas]]></source>
<year>2011</year>
<publisher-loc><![CDATA[Austin, United States of America ]]></publisher-loc>
<publisher-name><![CDATA[The University Texas at Austin]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B23">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Hedlund]]></surname>
<given-names><![CDATA[C.A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Fault-propagation, ductile strain, and displacement-distance relationships]]></article-title>
<source><![CDATA[Journal of Structural Geology]]></source>
<year>1997</year>
<volume>19</volume>
<numero>3-4</numero>
<issue>3-4</issue>
<page-range>249-56</page-range></nlm-citation>
</ref>
<ref id="B24">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Imlay]]></surname>
<given-names><![CDATA[R.W.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Evolution of the Coahuila Peninsula, Mexico. Geology of the Western Part of the Sierra de Parras]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>1936</year>
<numero>47</numero>
<issue>47</issue>
<page-range>1091-152</page-range></nlm-citation>
</ref>
<ref id="B25">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Johnson]]></surname>
<given-names><![CDATA[A.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Fletcher]]></surname>
<given-names><![CDATA[R.C.]]></given-names>
</name>
</person-group>
<source><![CDATA[Folding of viscous layers]]></source>
<year>1994</year>
<publisher-loc><![CDATA[New York ]]></publisher-loc>
<publisher-name><![CDATA[Columbia University Press]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B26">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Kelly]]></surname>
<given-names><![CDATA[W.A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Evolution of the Coahuila Peninsula, Mexico. Geology of the Mountains Bordering the Valleys of Acatita and Las Delicias]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>1936</year>
<numero>47</numero>
<issue>47</issue>
<page-range>1009-38</page-range></nlm-citation>
</ref>
<ref id="B27">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Lisle]]></surname>
<given-names><![CDATA[R.J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Strain estimation from flattened buckle folds]]></article-title>
<source><![CDATA[Journal of Structural Geology]]></source>
<year>1992</year>
<volume>14</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>369-71</page-range></nlm-citation>
</ref>
<ref id="B28">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Lugo-Hubp]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[El relieve de la República Mexicana]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>1990</year>
<volume>9</volume>
<page-range>82-111</page-range></nlm-citation>
</ref>
<ref id="B29">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[McKee]]></surname>
<given-names><![CDATA[J.W.]]></given-names>
</name>
<name>
<surname><![CDATA[Jones]]></surname>
<given-names><![CDATA[N.W.]]></given-names>
</name>
<name>
<surname><![CDATA[Long]]></surname>
<given-names><![CDATA[L.E.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Stratigraphy and provenance of strata along the San Marcos fault, central Coahuila, Mexico]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>1990</year>
<numero>102</numero>
<issue>102</issue>
<page-range>593-614</page-range></nlm-citation>
</ref>
<ref id="B30">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Ramsay]]></surname>
<given-names><![CDATA[J.G.]]></given-names>
</name>
</person-group>
<source><![CDATA[Folding and Fracturing of Rocks]]></source>
<year>1967</year>
<publisher-loc><![CDATA[New York ]]></publisher-loc>
<publisher-name><![CDATA[McGraw-Hill]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B31">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Ramsay]]></surname>
<given-names><![CDATA[J.G.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Development of Chevron Folds]]></article-title>
<source><![CDATA[Geological Society of America Bulletin]]></source>
<year>1974</year>
<numero>85</numero>
<issue>85</issue>
<page-range>1741-54</page-range></nlm-citation>
</ref>
<ref id="B32">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Rowan]]></surname>
<given-names><![CDATA[M.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Ratliff]]></surname>
<given-names><![CDATA[R.A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Use of fault cut-offs and bed travel distance in balanced cross-sections: Discussion 1]]></article-title>
<source><![CDATA[Journal of Structural Geology]]></source>
<year>1988</year>
<volume>10</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>311-6</page-range></nlm-citation>
</ref>
<ref id="B33">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Suppe]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Geometry and kinematics of fault- bend folding]]></article-title>
<source><![CDATA[American Journal of science]]></source>
<year>1983</year>
<numero>283</numero>
<issue>283</issue>
<page-range>684-721</page-range></nlm-citation>
</ref>
<ref id="B34">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Suppe]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Medwedeff]]></surname>
<given-names><![CDATA[D.A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Geometry and kinematics of fault-propagation folding]]></article-title>
<source><![CDATA[Eclogae Geologicae Helvetiae]]></source>
<year>1990</year>
<volume>83</volume>
<numero>3</numero>
<issue>3</issue>
<page-range>409-54</page-range></nlm-citation>
</ref>
<ref id="B35">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Vásquez-Serrano]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<source><![CDATA[Estimación de acortamiento a través del análisis de pliegues tipo chevron en la sección Vizarrón-Tamazunchale: Estados de Querétaro, Hidalgo y San Luis Potosí]]></source>
<year>2010</year>
<publisher-loc><![CDATA[Puebla, México ]]></publisher-loc>
<publisher-name><![CDATA[Benemérita Universidad Autónoma de Puebla]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B36">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Vásquez-Serrano]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Tolson]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Diaz]]></surname>
<given-names><![CDATA[E.F.]]></given-names>
</name>
<name>
<surname><![CDATA[Cabello]]></surname>
<given-names><![CDATA[G.C.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Influence of pre-tectonic carbonate facies architecture on deformation patterns of syntectonic turbidites, an example from the central Mexican fold-thrust belt]]></article-title>
<source><![CDATA[Journal of Structural Geology]]></source>
<year>2018</year>
<numero>109</numero>
<issue>109</issue>
<page-range>127-39</page-range></nlm-citation>
</ref>
<ref id="B37">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Williams]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Chapman]]></surname>
<given-names><![CDATA[T.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Strains developed in the hangingwalls of thrusts due to their slip/propagation rate: A dislocation model]]></article-title>
<source><![CDATA[Journal of Structural Geology]]></source>
<year>1983</year>
<volume>5</volume>
<numero>6</numero>
<issue>6</issue>
<page-range>563-71</page-range></nlm-citation>
</ref>
</ref-list>
</back>
</article>
