<?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>0122-5383</journal-id>
<journal-title><![CDATA[CT&F - Ciencia, Tecnología y Futuro]]></journal-title>
<abbrev-journal-title><![CDATA[C.T.F Cienc. Tecnol. Futuro]]></abbrev-journal-title>
<issn>0122-5383</issn>
<publisher>
<publisher-name><![CDATA[Instituto Colombiano del Petróleo (ICP) - ECOPETROL S.A.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0122-53832018000200083</article-id>
<article-id pub-id-type="doi">10.29047/01225383.84</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[FULL WAVEFORM INVERSION IN GENERALIZED COORDINATES FOR ZONES OF CURVED TOPOGRAPHY]]></article-title>
<article-title xml:lang="es"><![CDATA[USO DE LA INVERSIÓN DE ONDA COMPLETA (FWI) EN COORDENADAS GENERALIZADAS PARA ZONAS DE TOPOGRAFÍA IRREGULAR]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arias]]></surname>
<given-names><![CDATA[César]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Abreo]]></surname>
<given-names><![CDATA[David]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Abreo]]></surname>
<given-names><![CDATA[Sergio-Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Duque]]></surname>
<given-names><![CDATA[Luis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ramírez]]></surname>
<given-names><![CDATA[Ana-B]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Instituto Tecnológico Metropolitano  ]]></institution>
<addr-line><![CDATA[Medellín ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Industrial de Santander  ]]></institution>
<addr-line><![CDATA[Bucaramanga ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2018</year>
</pub-date>
<volume>8</volume>
<numero>2</numero>
<fpage>83</fpage>
<lpage>88</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0122-53832018000200083&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0122-53832018000200083&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0122-53832018000200083&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Full waveform inversion (FWI) has been recently used to estimate subsurface parameters, such as velocity models. This method, however, has a number of drawbacks when applied to zones with rugged topography due to the forced application of a Cartesian mesh on a curved surface. In this work, we present a simple coordinate transformation that enables the construction of a curved mesh. The proposed transformation is more suitable for rugged surfaces and it allows mapping a physical curved domain into a uniform rectangular grid, where acoustic FWI can be applied in the traditional way by introducing a modified Laplacian. We prove that the proposed approximation can have a wide range of applications, producing precise near-surface velocity models without increasing the computing time of the FWI.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La inversión de onda completa (FWI) ha sido usada recientemente para estimar parámetros del subsuelo, tal como modelos de velocidad. Este método sin embargo, tiene diferentes inconvenientes cuando se aplica a zonas con topografía abrupta debido a la aplicación forzada de una malla cartesiana sobre una superficie curvada. En este trabajo, presentamos una transformación de coordenadas simple que posibilita la construcción de una malla curvada. La transformación propuesta es más apropiada para superficies abruptas y permite mapear un dominio físico curvado a una malla rectangular uniforme, donde la FWI acústica puede ser aplicada de la manera tradicional introduciendo un Laplaciano modificado. Nosotros sugerimos que la aproximación propuesta puede tener un amplio rango de aplicaciones, produciendo modelos de velocidad precisos cerca a la superficie sin incrementar el tiempo de cómputo.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Full Wave Form Inversion]]></kwd>
<kwd lng="en"><![CDATA[Reverse Time Migration]]></kwd>
<kwd lng="en"><![CDATA[Rugged topography]]></kwd>
<kwd lng="en"><![CDATA[Velocity estimation]]></kwd>
<kwd lng="en"><![CDATA[Acoustic wave equation]]></kwd>
<kwd lng="es"><![CDATA[Inversión de Onda Completa]]></kwd>
<kwd lng="es"><![CDATA[Migración en Tiempo Inverso]]></kwd>
<kwd lng="es"><![CDATA[Topografía abrupta]]></kwd>
<kwd lng="es"><![CDATA[Estimación de velocidades]]></kwd>
<kwd lng="es"><![CDATA[Ecuación de onda acústica]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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