<?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>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742021000100018</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2021.1.1597</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Using electrical resistivity tomography to evaluate the relationship between groundwater potential and tectonism in northeast Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Empleo de Tomografía de Resistividad Eléctrica para evaluar la relación entre el potencial de agua subterránea y las condiciones tectónicas del noreste de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Batista-Rodríguez]]></surname>
<given-names><![CDATA[José Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-Flores]]></surname>
<given-names><![CDATA[Marco Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Almaguer-Carmenates]]></surname>
<given-names><![CDATA[Yuri]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Blanco-Moreno]]></surname>
<given-names><![CDATA[Jesús Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López-Saucedo]]></surname>
<given-names><![CDATA[Felipe de Jesús]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Batista-Cruz]]></surname>
<given-names><![CDATA[Ramón Yosvanis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Coahuila Escuela Superior de Ingeniería ]]></institution>
<addr-line><![CDATA[Nueva Rosita Coahuila]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Centro de Investigación Científica y de Educación Superior de Ensenada División de Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></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>38</volume>
<numero>1</numero>
<fpage>18</fpage>
<lpage>28</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742021000100018&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742021000100018&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742021000100018&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The relationship between groundwater potential and tectonic conditions in three sectors of clastic and carbonated sedimentary rocks of northeastern Mexico was identified using electrical resistivity tomography performed in seven transects. The electrical resistivity data were measured using Schlumberger, Wenner and dipole-dipole arrays of the electrodes. Subsequently, the data obtained were combined to carry out a 2D inversion. From interpretation of the electrical resistivity tomography data, several aquifers are located and characterized within varying thicknesses of conglomerates, sandstones and limestones. Additionally, fractures, faults and boundaries between rock types are identified in the obtained 2D models. These structural elements indicate that the aquifers have a strong relationship with the tectonism of the region. Depressed and uplifted blocks are generated through normal faults. The orientations of the inferred fractures and faults fit the structural characteristics of the study region. The aquifers are classified as semi-confined and confined. In clastic materials, these aquifers are classified as granular, while in limestone, they are mainly fractured. Fracture zones that connect most of the aquifers and connect the aquifers with the ground surface are also identified using electrical resistivity tomography. These zones can constitute the main recharge (including contamination) paths to the aquifers. This pollution can be related to livestock and industrial activities, as well as agriculture and mining in the region. Using these results, water wells were drilled to corroborate the identified aquifers.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Se presenta la relación entre el potencial de agua subterránea y las condiciones tectónicas en tres sectores de rocas sedimentarias clásticas y carbonatadas del noreste de México, utilizando tomografía de resistividad eléctrica en siete transectos. Los datos de resistividad eléctrica se tomaron usando arreglos Schlumberger, Wenner y dipolo-dipolo. Para realizar la inversión 2D, se combinaron los tres conjuntos de datos obtenidos. A partir de la interpretación de los datos de tomografía de resistividad eléctrica se localizaron y caracterizaron varios acuíferos dentro de diferentes espesores de conglomerado, arenisca y caliza. También, en el modelo 2D se identifican fracturas, fallas y límites entre tipos de rocas. Esos elementos estructurales indican que los acuíferos tienen una gran relación con el tectonismo de la región. Bloques hundidos y elevados se presentan asociados a fallas normales. La orientación de las fracturas y fallas inferidas se ajustan a las características estructurales de la región de estudio. Los acuíferos se clasifican como semi-confinados y confinados. En materiales clásticos, estos acuíferos se clasifican como granulares, mientras que en calizas son principalmente fracturados. En las tomografías también se identifican zonas de fracturas que conectan a la mayoría de los acuíferos y, a estos, con la superficie. Esas zonas pueden constituir las principales vías de recarga y contaminación de los acuíferos. La contaminación puede estar relacionada con las actividades ganaderas e industriales, así como con la agricultura y la minería en la región. Usando estos resultados se perforan pozos de agua para corroborar los acuíferos identificados.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[electrical resistivity tomography]]></kwd>
<kwd lng="en"><![CDATA[aquifers]]></kwd>
<kwd lng="en"><![CDATA[sedimentary rocks]]></kwd>
<kwd lng="en"><![CDATA[northeastern Mexico]]></kwd>
<kwd lng="es"><![CDATA[tomografía de resistividad eléctrica]]></kwd>
<kwd lng="es"><![CDATA[acuíferos]]></kwd>
<kwd lng="es"><![CDATA[rocas sedimentarias]]></kwd>
<kwd lng="es"><![CDATA[noreste de México]]></kwd>
</kwd-group>
</article-meta>
</front><back>
<ref-list>
<ref id="B1">
<nlm-citation citation-type="">
<collab>Advanced Geosciences, Inc</collab>
<source><![CDATA[Manual de Instrucciones para SuperSting TM con sistema de resistividad automática SwiftTM y PI. SuperSting R1/PI versión 01.01.38]]></source>
<year>2006</year>
<page-range>87</page-range></nlm-citation>
</ref>
<ref id="B2">
<nlm-citation citation-type="">
<collab>Advanced Geosciences, Inc</collab>
<source><![CDATA[Instruction Manual for EarthImager. Version 2.4.0. Resistivity and IP Inversion Software]]></source>
<year>2009</year>
<page-range>139</page-range></nlm-citation>
</ref>
<ref id="B3">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Armenta-Román]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Guzmán-Lugo]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Gómez-Nava]]></surname>
<given-names><![CDATA[J.A.]]></given-names>
</name>
<name>
<surname><![CDATA[Armenta de la Cruz]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
</person-group>
<source><![CDATA[Carta geológico-minera La Victoria G13-B49. Coahuila]]></source>
<year>2014</year>
<publisher-name><![CDATA[Servicio Geológico Mexicano]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B4">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Barriga-Paria]]></surname>
<given-names><![CDATA[Ch.J.]]></given-names>
</name>
<name>
<surname><![CDATA[Barriga-Gamarra]]></surname>
<given-names><![CDATA[J.P.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Identification and evaluation of fractures using electrical resistivity tomography in the vecinity of the axis of the Huamantanga Dam - Lima - Peru]]></article-title>
<source><![CDATA[Revista Brasileira de Geofísica]]></source>
<year>2018</year>
<volume>36</volume>
<numero>2</numero>
<issue>2</issue>
<page-range>111-22</page-range></nlm-citation>
</ref>
<ref id="B5">
<nlm-citation citation-type="book">
<collab>Comisión Nacional del Agua</collab>
<source><![CDATA[Actualización de la disponibilidad media anual de agua en el acuífero Cuatrociénegas-Ocampo (0504) Estado de Coahuila]]></source>
<year>2015</year>
<publisher-name><![CDATA[Subdirección General Técnica. Gerencia de Aguas Subterráneas, Subgerencia de Evaluación y Ordenamiento de acuíferos]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B6">
<nlm-citation citation-type="book">
<collab>Comisión Nacional del Agua</collab>
<source><![CDATA[Actualización de la disponibilidad media anual de agua anual en el acuífero Región Carbonífera (0512) Estado de Coahuila]]></source>
<year>2015</year>
<publisher-name><![CDATA[Subdirección General Técnica, Gerencia de Aguas Subterráneas. Subgerencia de Evaluación y Ordenamiento de acuíferos]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B7">
<nlm-citation citation-type="book">
<collab>Comisión Nacional del Agua</collab>
<source><![CDATA[Actualización de la disponibilidad media anual de agua anual en el acuífero Allende-Piedras Negras (0501) Estado de Coahuila]]></source>
<year>2015</year>
<publisher-name><![CDATA[Subdirección General Técnica, Gerencia de Aguas Subterráneas. Subgerencia de Evaluación y Ordenamiento de acuíferos]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B8">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Demirel]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Roubinet]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Irving]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Voytek]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Characterizing Near-Surface Fractured-Rock Aquifers: Insights Provided by the Numerical Analysis of Electrical Resistivity Experiments]]></article-title>
<source><![CDATA[Water]]></source>
<year>2018</year>
<volume>10</volume>
<numero>9</numero>
<issue>9</issue>
<page-range>2-20</page-range></nlm-citation>
</ref>
<ref id="B9">
<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>
<volume>75</volume>
<page-range>241-70</page-range></nlm-citation>
</ref>
<ref id="B10">
<nlm-citation citation-type="">
<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>
<person-group person-group-type="editor">
<name>
<surname><![CDATA[Bartolini]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Wilson]]></surname>
<given-names><![CDATA[J.L.]]></given-names>
</name>
<name>
<surname><![CDATA[Lawton]]></surname>
<given-names><![CDATA[T.F.]]></given-names>
</name>
</person-group>
<source><![CDATA[Mesozoic sedimentary and Tectonic History of North-Central Mexico]]></source>
<year>1999</year>
<volume>340</volume>
<page-range>1-58</page-range><publisher-loc><![CDATA[Boulder, Colorado, EUA ]]></publisher-loc>
</nlm-citation>
</ref>
<ref id="B11">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[González-Sánchez]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Puente-Solís]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[González-Partida]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Camprubí]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Estratigrafía del Noreste de México y su relación con los yacimientos estratoligados de fluorita, barita, celestina y Zn-Pb]]></article-title>
<source><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></source>
<year>2007</year>
<volume>59</volume>
<page-range>43-62</page-range></nlm-citation>
</ref>
<ref id="B12">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Gottardi]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Mason]]></surname>
<given-names><![CDATA[S.L.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Characterization of the natural fracture system of the Eagle Ford Formation (Val Verde County, Texas)]]></article-title>
<source><![CDATA[American Association of Petroleum Geologists Bulletin]]></source>
<year>2018</year>
<volume>102</volume>
<numero>10</numero>
<issue>10</issue>
<page-range>1963-84</page-range></nlm-citation>
</ref>
<ref id="B13">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Kovalevsky]]></surname>
<given-names><![CDATA[V.S.]]></given-names>
</name>
<name>
<surname><![CDATA[Kruseman]]></surname>
<given-names><![CDATA[G.P.]]></given-names>
</name>
<name>
<surname><![CDATA[Rushton]]></surname>
<given-names><![CDATA[K.R.]]></given-names>
</name>
</person-group>
<source><![CDATA[Groundwater studies. An international guide for hydrogeological investigations]]></source>
<year>2004</year>
<numero>3</numero>
<issue>3</issue>
<page-range>430</page-range><publisher-loc><![CDATA[Paris ]]></publisher-loc>
<publisher-name><![CDATA[UNESCO]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B14">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Nimnate]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Thitimakorn]]></surname>
<given-names><![CDATA[T.]]></given-names>
</name>
<name>
<surname><![CDATA[Choowong]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Hisada]]></surname>
<given-names><![CDATA[K]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Imaging and locationg paleo-channels using geophysical data from meandering system of the Mun River, Khorat Plateau, Northeastern Thailand]]></article-title>
<source><![CDATA[Open Geosciences]]></source>
<year>2017</year>
<volume>9</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>675-88</page-range></nlm-citation>
</ref>
<ref id="B15">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Obiadi]]></surname>
<given-names><![CDATA[I.I.]]></given-names>
</name>
<name>
<surname><![CDATA[Onwuemesi]]></surname>
<given-names><![CDATA[A.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Anike]]></surname>
<given-names><![CDATA[O.L.]]></given-names>
</name>
<name>
<surname><![CDATA[Obiadi]]></surname>
<given-names><![CDATA[C.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Ajaegwu]]></surname>
<given-names><![CDATA[N.E.]]></given-names>
</name>
<name>
<surname><![CDATA[Anakwuba]]></surname>
<given-names><![CDATA[E.K.]]></given-names>
</name>
<name>
<surname><![CDATA[Akpunonu]]></surname>
<given-names><![CDATA[E.O.]]></given-names>
</name>
<name>
<surname><![CDATA[Ezim]]></surname>
<given-names><![CDATA[E.O.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Imaging subsurface fracture characteristics using 2D electrical resistivity tomography]]></article-title>
<source><![CDATA[International Research Journal of Engineering Science, Technology and Innovation]]></source>
<year>2012</year>
<volume>1</volume>
<numero>4</numero>
<issue>4</issue>
<page-range>103-10</page-range></nlm-citation>
</ref>
<ref id="B16">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Padilla y Sánchez]]></surname>
<given-names><![CDATA[R.J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Post-Paleozoic Tectonics of Northeast Mexico and its role in the evolution of the Gulf of Mexico]]></article-title>
<source><![CDATA[Geofísica Internacional]]></source>
<year>1986</year>
<volume>25</volume>
<page-range>157-206</page-range></nlm-citation>
</ref>
<ref id="B17">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Raghunath]]></surname>
<given-names><![CDATA[H.M.]]></given-names>
</name>
</person-group>
<source><![CDATA[Hydrology: principles, analysis and design]]></source>
<year>2006</year>
<edition>Second</edition>
<page-range>463</page-range><publisher-loc><![CDATA[New Delhi, India ]]></publisher-loc>
<publisher-name><![CDATA[New Age International (P), Ltd., Publishers]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B18">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Ratnakumari]]></surname>
<given-names><![CDATA[Y.]]></given-names>
</name>
<name>
<surname><![CDATA[Rai]]></surname>
<given-names><![CDATA[S.N.]]></given-names>
</name>
<name>
<surname><![CDATA[Thiagarajan]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Kumar]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[2D electrical resistivity imaging for delineation of deeper aquifers in a part of the Chandrabhaga river basin, Nagpur District, Maharashtra, India]]></article-title>
<source><![CDATA[Current Science]]></source>
<year>2012</year>
<volume>102</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>61-9</page-range></nlm-citation>
</ref>
<ref id="B19">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Robert]]></surname>
<given-names><![CDATA[T.]]></given-names>
</name>
<name>
<surname><![CDATA[Dassargues]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Brouyère]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Kaufmann]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
<name>
<surname><![CDATA[Hallet]]></surname>
<given-names><![CDATA[V.]]></given-names>
</name>
<name>
<surname><![CDATA[Nguyen]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Assessing the contribution of electrical resistivity tomography (ERT) and self-potential (SP) methods for a water well drilling program in fractured/karsti&#64257;ed limestones]]></article-title>
<source><![CDATA[Journal of Applied Geophysics]]></source>
<year>2011</year>
<volume>75</volume>
<page-range>42-53</page-range></nlm-citation>
</ref>
<ref id="B20">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Sanchez]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Rodriguez]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Tortajada]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Transboundary aquifers between Chihuahua, Coahuila, Nuevo Leon and Tamaulipas, Mexico, and Texas, USA: Identification and Categorization]]></article-title>
<source><![CDATA[Journal of Hydrology: Regional Studies]]></source>
<year>2018</year>
<volume>20</volume>
<page-range>74-102</page-range></nlm-citation>
</ref>
<ref id="B21">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Santiago-Carrasco]]></surname>
<given-names><![CDATA[B.]]></given-names>
</name>
<name>
<surname><![CDATA[Ontiveros-Escobedo]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Martínez-Rodríguez]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Herrera-Monreal]]></surname>
<given-names><![CDATA[J.C.]]></given-names>
</name>
</person-group>
<source><![CDATA[Carta geológico-minera Piedras Negras H14-10. Coahuila]]></source>
<year>2008</year>
<publisher-name><![CDATA[Servicio Geológico Mexicano]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B22">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Sequeira-Gómez]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Escolero-Fuentes]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[The application of electrical methods in exploration for ground water resources in the River Malacatoya sub-basin, Nicaragua]]></article-title>
<source><![CDATA[Geofísica Internacional]]></source>
<year>2010</year>
<volume>49</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>27-41</page-range></nlm-citation>
</ref>
<ref id="B23">
<nlm-citation citation-type="">
<collab>Servicio Geológico Mexicano</collab>
<source><![CDATA[Carta geológico-minera Nueva Rosita Coahuila G14-13]]></source>
<year>2003</year>
</nlm-citation>
</ref>
<ref id="B24">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Srinivasamoorthy]]></surname>
<given-names><![CDATA[K.]]></given-names>
</name>
<name>
<surname><![CDATA[Sarma]]></surname>
<given-names><![CDATA[VS.]]></given-names>
</name>
<name>
<surname><![CDATA[Vasantavigar]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Vijayaraghavan]]></surname>
<given-names><![CDATA[K.]]></given-names>
</name>
<name>
<surname><![CDATA[Chidambaram]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Rajivganthi]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Electrical imaging techniques for groundwater pollution studies: a case study from Tamil Nadu state, south India]]></article-title>
<source><![CDATA[Earth Sciences Research Journal]]></source>
<year>2009</year>
<volume>13</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>30-9</page-range></nlm-citation>
</ref>
<ref id="B25">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Szalai]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Kovács]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Kuslits]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
<name>
<surname><![CDATA[Facskó]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Gribovszki]]></surname>
<given-names><![CDATA[K.]]></given-names>
</name>
<name>
<surname><![CDATA[Kalmár]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Szarka]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Characterisation of Fractures and Fracture Zones in a Carbonate Aquifer Using Electrical Resistivity Tomography and Pricking Probe Methodes]]></article-title>
<source><![CDATA[Journal of Geoscience and Environment Protection]]></source>
<year>2018</year>
<volume>6</volume>
<numero>4</numero>
<issue>4</issue>
<page-range>1-21</page-range></nlm-citation>
</ref>
<ref id="B26">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Tangdamrongsub]]></surname>
<given-names><![CDATA[N.]]></given-names>
</name>
<name>
<surname><![CDATA[Steele-Dunne]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Gunter]]></surname>
<given-names><![CDATA[B.C.]]></given-names>
</name>
<name>
<surname><![CDATA[Ditmar]]></surname>
<given-names><![CDATA[P.G.]]></given-names>
</name>
<name>
<surname><![CDATA[Sutanudjaja]]></surname>
<given-names><![CDATA[E.H.]]></given-names>
</name>
<name>
<surname><![CDATA[Sun]]></surname>
<given-names><![CDATA[Y.]]></given-names>
</name>
<name>
<surname><![CDATA[Xia]]></surname>
<given-names><![CDATA[T.]]></given-names>
</name>
<name>
<surname><![CDATA[Wang]]></surname>
<given-names><![CDATA[Z.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Improving estimates of water resources in a semi-arid region by assimilating GRACE data into the PCR-GLOBWB hydrological model]]></article-title>
<source><![CDATA[Hydrology and Earth System Sciences]]></source>
<year>2017</year>
<volume>21</volume>
<page-range>2053-74</page-range></nlm-citation>
</ref>
<ref id="B27">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Telford]]></surname>
<given-names><![CDATA[W.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Geldart]]></surname>
<given-names><![CDATA[L.P.]]></given-names>
</name>
<name>
<surname><![CDATA[Sheriff]]></surname>
<given-names><![CDATA[R.E.]]></given-names>
</name>
</person-group>
<source><![CDATA[Applied Geophysics]]></source>
<year>1990</year>
<edition>Second</edition>
<page-range>792</page-range><publisher-name><![CDATA[Cambridge University Press]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B28">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Winker]]></surname>
<given-names><![CDATA[C.D.]]></given-names>
</name>
<name>
<surname><![CDATA[Buf&#64258;er]]></surname>
<given-names><![CDATA[R.T.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Paleogeographic evolution of earlydeep-water Gulf of Mexico and margins, Jurassic to Middle Cretaceous (Comanchean)]]></article-title>
<source><![CDATA[American Association of Petroleum Geologists Bulletin]]></source>
<year>1988</year>
<volume>72</volume>
<page-range>318-46</page-range></nlm-citation>
</ref>
<ref id="B29">
<nlm-citation citation-type="book">
<collab>World Meteorological Organization</collab>
<source><![CDATA[Guide to Hydrological Practices. Volume II. Management of water resources and application of hydrological practices]]></source>
<year>2009</year>
<numero>168</numero>
<edition>Sixt</edition>
<issue>168</issue>
<page-range>302</page-range><publisher-loc><![CDATA[Switzerland ]]></publisher-loc>
<publisher-name><![CDATA[WMO]]></publisher-name>
</nlm-citation>
</ref>
</ref-list>
</back>
</article>
