<?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>0122-3461</journal-id>
<journal-title><![CDATA[Ingeniería y Desarrollo]]></journal-title>
<abbrev-journal-title><![CDATA[Ing. Desarro.]]></abbrev-journal-title>
<issn>0122-3461</issn>
<publisher>
<publisher-name><![CDATA[Fundación Universidad del Norte]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0122-34612025000200277</article-id>
<article-id pub-id-type="doi">10.14482/inde.43.02.986.861</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Producción y caracterización geoquímica del gas en la cuenca Valle Inferior del Magdalena (Colombia). Implicaciones en la prospectividad del gas natural y el gas licuado del petróleo]]></article-title>
<article-title xml:lang="en"><![CDATA[Production and geochemical characterization of gas in the Lower Magdalena basin (Colombia). Implications for natural gas and liquefied petroleum gas prospectivity]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[MORA HERNÁNDEZ]]></surname>
<given-names><![CDATA[CÉSAR AUGUSTO]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[POSADA SALDARRIAGA]]></surname>
<given-names><![CDATA[CLAUDIA ROSA]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[SILVEIRA MORENO]]></surname>
<given-names><![CDATA[GLEUBIS BELÉN]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[CHAJÍN ORTIZ]]></surname>
<given-names><![CDATA[PATRICIA]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[&#1042;ERMÚDEZ]]></surname>
<given-names><![CDATA[MAURICIO]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Federal Río de Janeiro  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional de Colombia  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Pedagógica y Tecnológica de Colombia  ]]></institution>
<addr-line><![CDATA[Sogamoso ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Industrial de Santander  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Université Joseph Fourier  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>France</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2025</year>
</pub-date>
<volume>43</volume>
<numero>2</numero>
<fpage>277</fpage>
<lpage>299</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0122-34612025000200277&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0122-34612025000200277&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0122-34612025000200277&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En la cuenca Valle Inferior del Magdalena (VIM) se han descubierto hasta la fecha 1201 MBPE (OOIP &amp; OGIP/ crudo y gas). Los recursos de gas descubiertos alcanzan 3,57 TPC e incluyen gas seco y gas húmedo. Durante 2021, la ANH (Agencia Nacional de Hidrocarburos) fiscalizó la producción de 29 campos con una producción total de 90908 MPC (99,91 GPCG), los cuales representan el 15 % del total producido en el país. Los principales reservorios en la cuenca corresponden a facies arenosas de la Formación Ciénaga de Oro Inferior (Oligoceno tardío) y facies calcáreas de la Formación Ciénaga de Oro Superior (Mioceno temprano). El gas producido varía entre seco, con más de 98 % de metano, y húmedo, en el que la proporción de GLP (C3+) es mayor al 5 %. Con base en la caracterización geoquímica, los gases húmedos se asocian a craqueo primario del kerógeno y los gases secos a craqueo secundario de crudo. La presencia en la cuenca de un amplio espectro de hidrocarburos líquidos y gaseosos representa una oportunidad exploratoria, ya que se trata de una cuenca donde es posible encontrar gas natural (GN / C1) y gas húmedo (C3-C5), este último es considerado como fuente principal del gas licuado del petróleo (GLP).]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract In the Lower Magdalena Valley (VIM) basin, 1201 MBPE have been discovered (OOIP &amp; OGIP/ oil and gas). Gas resources discovered reach 3.57 TPC and include dry gas and wet gas. During 2021 the ANH (Agencia Nacional de Hidrocarburos) audited the production of 29 fields with a total production of 90908 MPC (99.91 GPCG), which accounts for 15 % of total production in the country. The main reservoirs in the basin correspond to sandy facies of the Lower Ciénaga de Oro Formation (late Oligocene) and calcareous facies of the Upper Ciénaga de Oro Formation (early Miocene). The gas produced varies between dry with more than 98% methane and humid where the proportion of LPG (C3+) is greater than 5%. Based on the geochemical characterization, wet gases are associated with primary kerogen cracking, and dry gases with secondary crude oil cracking. The presence in the basin of a wide spectrum of liquid and gaseous hydrocarbons represents an exploratory opportunity, since it is a basin where it is possible to find natural gas (NG/ C1) and wet gas (C3-C5), the main source of liquefied petroleum gas (LPG).]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[composición molecular e isotópica]]></kwd>
<kwd lng="es"><![CDATA[craqueo]]></kwd>
<kwd lng="es"><![CDATA[gas seco]]></kwd>
<kwd lng="es"><![CDATA[gas húmedo]]></kwd>
<kwd lng="es"><![CDATA[producción de gas]]></kwd>
<kwd lng="en"><![CDATA[cracking]]></kwd>
<kwd lng="en"><![CDATA[dry gas]]></kwd>
<kwd lng="en"><![CDATA[gas production]]></kwd>
<kwd lng="en"><![CDATA[molecular and isotopic composition]]></kwd>
<kwd lng="en"><![CDATA[wet gas]]></kwd>
</kwd-group>
</article-meta>
</front><back>
<ref-list>
<ref id="B1">
<label>[1]</label><nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Mora]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Posada]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Osorno]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Evaluación de los recursos de hidrocarburos remanentes en Colombia (Yet to find)", Agencia Nacional de Hidrocarburos, Plan 2020]]></article-title>
<source><![CDATA[Aportes a la exploración de hidrocarburos en Colombia]]></source>
<year>2020</year>
<page-range>16-22</page-range><publisher-loc><![CDATA[Bogotá ]]></publisher-loc>
</nlm-citation>
</ref>
<ref id="B2">
<label>[2]</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Pardo]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Mora]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Gallego]]></surname>
<given-names><![CDATA[N.]]></given-names>
</name>
</person-group>
<source><![CDATA[Evolución geológica, sistemas petrolíferos y prospectividad del gas en la subcuenca Plato (Valle Inferior del Magdalena)]]></source>
<year>2020</year>
<page-range>76-144</page-range><publisher-loc><![CDATA[Bogotá, D. C. ]]></publisher-loc>
<publisher-name><![CDATA[Agencia Nacional de Hidrocarburos]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B3">
<label>[3]</label><nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Pardo]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Mora]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Gallego]]></surname>
<given-names><![CDATA[N.]]></given-names>
</name>
<name>
<surname><![CDATA[Arenas]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Echeverry]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<name>
<surname><![CDATA[Osorno]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA["Potencial petrolífero en la Sub-cuenca de Plato (Valle Inferior del Magdalena, Caribe colombiano)". Agencia Nacional de Hidrocarburos, Plan 2020]]></article-title>
<source><![CDATA[Aportes a la exploración de hidrocarburos en Colombia]]></source>
<year>2020</year>
<page-range>98-110</page-range><publisher-loc><![CDATA[Bogotá, D. C. ]]></publisher-loc>
</nlm-citation>
</ref>
<ref id="B4">
<label>[4]</label><nlm-citation citation-type="">
<collab>Agencia Nacional de Hidrocarburos</collab>
<article-title xml:lang=""><![CDATA[Producción Fiscalizada Gas 2021]]></article-title>
<source><![CDATA[Operaciones y Regalías, Sistemas Integrados de Operaciones, Estadísticas de producción]]></source>
<year>2022</year>
</nlm-citation>
</ref>
<ref id="B5">
<label>[5]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Montes]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Bayona]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Cardona]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Valencia]]></surname>
<given-names><![CDATA[V.]]></given-names>
</name>
<name>
<surname><![CDATA[Jaramillo]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Clockwise rotation of the Santa Marta massif and simultaneous Paleogene to Neogene deformation of the Plato-San Jorge and Cesar-Rancheria basins]]></article-title>
<source><![CDATA[Journal of South American Earth Sciences]]></source>
<year>2010</year>
<volume>29</volume>
<numero>4</numero>
<issue>4</issue>
<page-range>832-48</page-range></nlm-citation>
</ref>
<ref id="B6">
<label>[6]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Mora]]></surname>
<given-names><![CDATA[J.A.]]></given-names>
</name>
<name>
<surname><![CDATA[Oncken]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
<name>
<surname><![CDATA[Breton]]></surname>
<given-names><![CDATA[E. Le]]></given-names>
</name>
<name>
<surname><![CDATA[Mora]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Veloza]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<name>
<surname><![CDATA[Vélez]]></surname>
<given-names><![CDATA[V.]]></given-names>
</name>
<name>
<surname><![CDATA[de Freitas]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Controls on forearc basin formation and evolution: Insights from Oligocene to Recent tectono-stratigraphy of the Lower Magdalena Valley basin of northwest Colombia]]></article-title>
<source><![CDATA[Marine and Petroleum Geology]]></source>
<year>2018</year>
<volume>97</volume>
<page-range>288-310</page-range></nlm-citation>
</ref>
<ref id="B7">
<label>[7]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Reyes]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[Montenegro]]></surname>
<given-names><![CDATA[B.]]></given-names>
</name>
<name>
<surname><![CDATA[Gómez]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Tectonoestratigrafía y evolución geológica del Valle Inferior del Magdalena]]></article-title>
<source><![CDATA[BoL GeoL]]></source>
<year>2004</year>
<volume>26</volume>
<numero>42</numero>
<issue>42</issue>
<page-range>19-38</page-range></nlm-citation>
</ref>
<ref id="B8">
<label>[8]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Bernal-Olaya]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Mann]]></surname>
<given-names><![CDATA[P.]]></given-names>
</name>
<name>
<surname><![CDATA[Escalona]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Cenozoic tectonostratigraphic evolution of the Lower Magdalena Basin, Colombia: An example of an under-to overfilled forearc basin]]></article-title>
<source><![CDATA[Memoir 108: Petroleum Geology and Potential of the Colombian Caribbean Margin]]></source>
<year>2015</year>
<volume>108</volume>
<page-range>345-98</page-range></nlm-citation>
</ref>
<ref id="B9">
<label>[9]</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Guzman]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
</person-group>
<source><![CDATA[Stratigraphy and sedimentary environment and implications in the Plato Basin and San Jacinto Belt Northwestern Colombia]]></source>
<year>2007</year>
<publisher-name><![CDATA[Univ. de Liège]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B10">
<label>[10]</label><nlm-citation citation-type="confpro">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Bermúdez]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
</person-group>
<source><![CDATA[Esquema estratigráfico de secuencias del registro sedimentario del Cinturón Plegado de San Jacinto, Caribe colombiano]]></source>
<year>2016</year>
<conf-name><![CDATA[ XIISimposio Bolivariano Exploración Petrolera en Cuencas Subandinas]]></conf-name>
<conf-loc> </conf-loc>
<page-range>3-11</page-range></nlm-citation>
</ref>
<ref id="B11">
<label>[11]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Mora]]></surname>
<given-names><![CDATA[J.A.]]></given-names>
</name>
<name>
<surname><![CDATA[Ibáñez-Mejía]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<name>
<surname><![CDATA[Oncken]]></surname>
<given-names><![CDATA[O.]]></given-names>
</name>
<name>
<surname><![CDATA[Freitas]]></surname>
<given-names><![CDATA[M. De]]></given-names>
</name>
<name>
<surname><![CDATA[Vélez]]></surname>
<given-names><![CDATA[V.]]></given-names>
</name>
<name>
<surname><![CDATA[Mesa]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Serna]]></surname>
<given-names><![CDATA[L.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Structure and age of the lower Magdalena valley basement, northern Colombia: new reflection-seismic and U-Pb-Hf insights into the termination of the central Andes against the Caribbean basin]]></article-title>
<source><![CDATA[Journal of South American Earth Sciences]]></source>
<year>2017</year>
<volume>74</volume>
<page-range>1-26</page-range></nlm-citation>
</ref>
<ref id="B12">
<label>[12]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Aguilera]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Sotelo]]></surname>
<given-names><![CDATA[V.]]></given-names>
</name>
<name>
<surname><![CDATA[Burgos]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Arce]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Gómez]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<name>
<surname><![CDATA[Mojica]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<name>
<surname><![CDATA[Castillo]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[Jiménez]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
<name>
<surname><![CDATA[Osorno]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Organic Geochemistry Atlas of Colombia]]></article-title>
<source><![CDATA[Earth Sciences Research Journal]]></source>
<year></year>
<volume>14</volume>
<numero>^sSpecial Edition</numero>
<issue>^sSpecial Edition</issue>
<supplement>Special Edition</supplement>
<page-range>102-12</page-range></nlm-citation>
</ref>
<ref id="B13">
<label>[13]</label><nlm-citation citation-type="book">
<collab>UPTC-ANH</collab>
<source><![CDATA[Evaluación de la prospectividad del gas en Colombia en las cuencas onshore con producción comercial]]></source>
<year>2021</year>
<page-range>453-61</page-range><publisher-loc><![CDATA[Bogotá, D. C ]]></publisher-loc>
<publisher-name><![CDATA[Agencia Nacional de Hidrocarburos]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B14">
<label>[14]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Schoell]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Genetic characterization of natural gases]]></article-title>
<source><![CDATA[AAPGBulletin]]></source>
<year>1983</year>
<volume>67</volume>
<numero>12</numero>
<issue>12</issue>
<page-range>2225-38</page-range></nlm-citation>
</ref>
<ref id="B15">
<label>[15]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Prinzhofer]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Pernaton]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Isotopically light in natural gas: bacterial imprint or diffusive fractionation]]></article-title>
<source><![CDATA[Chemistry and Geology]]></source>
<year>1997</year>
<volume>142</volume>
<numero>3-4</numero>
<issue>3-4</issue>
<page-range>193-200</page-range></nlm-citation>
</ref>
<ref id="B16">
<label>[16]</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Zhiyong]]></surname>
<given-names><![CDATA[H.]]></given-names>
</name>
<name>
<surname><![CDATA[Murray]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Moore]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
</person-group>
<source><![CDATA[Top-Down Petroleum Systems Analysis: Prediction of Petroleum Phase and Properties]]></source>
<year>2021</year>
<publisher-loc><![CDATA[London ]]></publisher-loc>
<publisher-name><![CDATA[The Geological Society]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B17">
<label>[17]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Khaled]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<name>
<surname><![CDATA[Arouri Herrera]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Phase envelopes in reservoir fill analysis: Two contrasting scenarios]]></article-title>
<source><![CDATA[Scientific Reports]]></source>
<year>2024</year>
<volume>14</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>5601</page-range></nlm-citation>
</ref>
<ref id="B18">
<label>[18]</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Tissot]]></surname>
<given-names><![CDATA[B. P.]]></given-names>
</name>
<name>
<surname><![CDATA[Welte]]></surname>
<given-names><![CDATA[D.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Production and Accumulation of Organic Matter]]></article-title>
<source><![CDATA[Petroleum Formation and Occurrence]]></source>
<year>1984</year>
<publisher-loc><![CDATA[New York, NY ]]></publisher-loc>
<publisher-name><![CDATA[Springer-Verlag]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B19">
<label>[19]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[García]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Galván]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
<name>
<surname><![CDATA[Samaniego]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Comportamiento termodinámico de los yacimientos de gas seco, gas húmedo y gas y condensado]]></article-title>
<source><![CDATA[Ingeniería Petrolera]]></source>
<year>2019</year>
<volume>59</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>4-21</page-range></nlm-citation>
</ref>
<ref id="B20">
<label>[20]</label><nlm-citation citation-type="book">
<collab>UPTC-MINCIENCIAS-ANH</collab>
<source><![CDATA[Hábitat geológico, prospectividad, sostenibilidad socioambiental y económica del gas húmedo (GLP) en Colombia como combustible de transición energética]]></source>
<year>2023</year>
<page-range>23-8</page-range><publisher-loc><![CDATA[Bogotá, D. C. ]]></publisher-loc>
<publisher-name><![CDATA[Agencia Nacional de Hidrocarburos]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B21">
<label>[21]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Lorant]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Prinzhofer]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Behar]]></surname>
<given-names><![CDATA[F.]]></given-names>
</name>
<name>
<surname><![CDATA[Huc]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Carbon isotopic and molecular constraints on the formation and the expulsion of thermogenic hydrocarbon gases]]></article-title>
<source><![CDATA[Chemical Geology]]></source>
<year>1998</year>
<volume>147</volume>
<numero>3-4</numero>
<issue>3-4</issue>
<page-range>249-64</page-range></nlm-citation>
</ref>
<ref id="B22">
<label>[22]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Rangel]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<name>
<surname><![CDATA[Katz]]></surname>
<given-names><![CDATA[B.]]></given-names>
</name>
<name>
<surname><![CDATA[Ramírez]]></surname>
<given-names><![CDATA[V.]]></given-names>
</name>
<name>
<surname><![CDATA[Vaz Dos Santos Neto]]></surname>
<given-names><![CDATA[E.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Alternative interpretations as to the Origin of the hydrocarbons of the Guajira Basin, Colombia]]></article-title>
<source><![CDATA[Mar. and Petroleum Geology]]></source>
<year>2003</year>
<volume>20</volume>
<numero>2</numero>
<issue>2</issue>
<page-range>129-39</page-range></nlm-citation>
</ref>
<ref id="B23">
<label>[23]</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Tobías]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Interpreters and near-field exploration: The role of leadership, culture, and organizational impedance contrasts]]></article-title>
<source><![CDATA[Interpretation]]></source>
<year>2018</year>
<volume>6</volume>
<numero>2</numero>
<issue>2</issue>
<page-range>5M-12M</page-range></nlm-citation>
</ref>
</ref-list>
</back>
</article>
