<?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>1409-2433</journal-id>
<journal-title><![CDATA[Revista de Matemática Teoría y Aplicaciones]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. Mat]]></abbrev-journal-title>
<issn>1409-2433</issn>
<publisher>
<publisher-name><![CDATA[Centro de Investigaciones en Matemática Pura y Aplicada (CIMPA) y Escuela de Matemática, San José, Costa Rica.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1409-24332012000100009</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Tsunami: Un problema matemáticamente interesante]]></article-title>
<article-title xml:lang="en"><![CDATA[Tsunami: An interesting mathematical problema]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González González]]></surname>
<given-names><![CDATA[Rodrigo]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortiz Figueroa]]></surname>
<given-names><![CDATA[Modesto]]></given-names>
</name>
<xref ref-type="aff" rid="A02"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Montoya Rodríguez]]></surname>
<given-names><![CDATA[José Miguel]]></given-names>
</name>
<xref ref-type="aff" rid="A03"/>
</contrib>
</contrib-group>
<aff id="A01">
<institution><![CDATA[,Universidad de Sonora Departamento de Matemáticas ]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>México</country>
</aff>
<aff id="A02">
<institution><![CDATA[,CICESE Departamento de Oceanografía Física ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>México</country>
</aff>
<aff id="A03">
<institution><![CDATA[,Instituto Mexicano del Transporte División de Ingeniería de Puertos y Costas ]]></institution>
<addr-line><![CDATA[ Querétaro]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>01</month>
<year>2012</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>01</month>
<year>2012</year>
</pub-date>
<volume>19</volume>
<numero>1</numero>
<fpage>107</fpage>
<lpage>119</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S1409-24332012000100009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S1409-24332012000100009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S1409-24332012000100009&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Se presentan algunos aspectos fundamentales respecto a la matemática y la herramienta computacional que apoyan la compleja descripción del proceso físico tsunami desde dos enfoques específicos. En particular, se aborda analíticamente un modelo hidroelástico simple para el problema de generación de ondas tsunami, el cual permite obtener resultados en el área de ruptura. Por otra parte, el proceso de propagación de las ondas tsunami en el océano y el impacto a lo largo de la línea costera se analiza numéricamente utilizando el enfoque hidrodinámico, presentando en particular una aplicación directa sobre la predicción de tsunamis en México producidos por sismos potenciales en la trinchera Mesoamericana mediante el diseño de un &#8220;Módulo Sintetizador de Tsunamis&#8221; para simular tsunamis originados por sismos ocurridos en la zona de subducción de la costa occidental de México.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[We present some key aspects regarding the mathematics and the computational tool that support the complex description of the physical process tsunami from two specific approaches. In particular, it addresses analytically a simple hydroelastic model for the problem of tsunami wave generation, which provides results in the rupture area. Moreover, the propagation of tsunami waves in the ocean and the impact along the coastline is analyzed numerically using the hydrodynamic approach, presenting in particular a direct application to the prediction of tsunamis in Mexico caused by potential earthquakes in the Mesoamerican trench through the design of a &#8220;Tsunami Toolbox&#8221; to simulate tsunamis caused by earthquakes in the subduction zone on the western coast of Mexico.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[ondas tsunami]]></kwd>
<kwd lng="es"><![CDATA[métodos matemáticos]]></kwd>
<kwd lng="es"><![CDATA[simulación]]></kwd>
<kwd lng="es"><![CDATA[tsunami]]></kwd>
<kwd lng="en"><![CDATA[waves]]></kwd>
<kwd lng="en"><![CDATA[mathematical methods]]></kwd>
<kwd lng="en"><![CDATA[simulation]]></kwd>
</kwd-group>
</article-meta>
</front><body><![CDATA[ <div style="text-align: justify;">     <div style="text-align: justify;">     <div style="text-align: center;"><font style="font-weight: bold;"  size="4"><span style="font-family: verdana;">Tsunami. Un problema matem&aacute;ticamente interesante</span></font><br  style="font-family: verdana;"> </div> <br style="font-family: verdana;">     <div style="text-align: center;"><font style="font-weight: bold;"  size="4"><span style="font-family: verdana;">Tsunami. An interesting mathematical problema</span></font><br style="font-family: verdana;"> </div> <br style="font-family: verdana;">     <div style="text-align: center;"><font size="2"><span  style="font-family: verdana;">Rodrigo Gonz&aacute;lez Gonz&aacute;lez<a href="#afiliacion1">*</a><a name="afiliacionh4"></a>+</span></font><font  size="2"><span style="font-family: verdana;"> Modesto Ortiz Figueroa<a href="#afiliacion2">&#8224;</a><a name="afiliacion5"></a>*</span></font><font  size="2"><span style="font-family: verdana;"> Jos&eacute; Miguel Montoya Rodr&iacute;guez<a href="#afiliacion3">&#8225;</a><a name="afiliacion6"></a>*</span></font><br  style="font-family: verdana;"> </div> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;"></span></font><font  size="2"><span style="font-family: verdana;">    <br>     <br> <a name="correspondencia2"></a>*<a href="#correspondencia1">Direccion para correspondencia</a></span></font><br style="font-family: verdana;"> <font style="font-weight: bold;" size="3"><span  style="font-family: verdana;"></span></font> <hr style="width: 100%; height: 2px;"><font style="font-weight: bold;"  size="3"><span style="font-family: verdana;">Resumen</span></font><br  style="font-family: verdana;"> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">Se presentan algunos aspectos fundamentales respecto a la matem&aacute;tica y la herramienta computacional que apoyan la compleja descripci&oacute;n del proceso f&iacute;sico tsunami desde dos enfoques espec&iacute;ficos. En particular, se aborda anal&iacute;ticamente un modelo hidroel&aacute;stico simple para el problema de generaci&oacute;n de ondas tsunami, el cual permite obtener resultados en el &aacute;rea de ruptura. Por otra parte, el proceso de propagaci&oacute;n de las ondas tsunami en el oc&eacute;ano y el impacto a lo largo de la l&iacute;nea costera se analiza num&eacute;ricamente utilizando el enfoque hidrodin&aacute;mico, presentando en particular una aplicaci&oacute;n directa sobre la predicci&oacute;n de tsunamis en M&eacute;xico producidos por sismos potenciales en la trinchera Mesoamericana mediante el dise&ntilde;o de un <span style="font-style: italic;">&#8220;M&oacute;dulo Sintetizador de Tsunamis&#8221;</span> para simular tsunamis originados por sismos ocurridos en la zona de subducci&oacute;n de la costa occidental de M&eacute;xico.</span></font><br  style="font-family: verdana;"> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;"><span  style="font-weight: bold;">Palabras clave:</span> ondas tsunami, m&eacute;todos matem&aacute;ticos, simulaci&oacute;n.</span></font><br  style="font-family: verdana;"> <br style="font-family: verdana;"> <font style="font-weight: bold;" size="3"><span  style="font-family: verdana;">Abstract</span></font><br  style="font-family: verdana;"> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">We present some key aspects regarding the mathematics and the computational tool that support the complex description of the physical process tsunami from two specific approaches. In particular, it addresses analytically a simple hydroelastic model for the problem of tsunami wave generation, which provides results in the rupture area. Moreover, the propagation of tsunami waves in the ocean and the impact along the coastline is analyzed numerically using the hydrodynamic approach, presenting in particular a direct application to the prediction of tsunamis in Mexico caused by potential earthquakes in the Mesoamerican trench through the design of a<span style="font-style: italic;"> &#8220;Tsunami Toolbox&#8221;</span> to simulate tsunamis caused by earthquakes in the subduction zone on the western coast of Mexico.</span></font><br  style="font-family: verdana;"> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;"><span  style="font-weight: bold;">Keywords:</span> tsunami waves, mathematical methods, simulation.</span></font><br  style="font-family: verdana;"> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;"><span  style="font-weight: bold;">Mathematics Subject Classification:</span> 76U05, 76V05.    <br> <br style="font-family: verdana;"> </span></font><font style="font-weight: bold;" size="3"><span  style="font-family: verdana;"></span></font> <hr style="width: 100%; height: 2px;">    <br> Ver contenido disponible en pdf    <br>     ]]></body>
<body><![CDATA[<br> <hr style="width: 100%; height: 2px;"><font style="font-weight: bold;"  size="3"><span style="font-family: verdana;">Agradecimientos</span></font><br  style="font-family: verdana;">     <br> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">La realizaci&oacute;n de la parte te&oacute;rica fue una primera actividad del proyecto: <span  style="font-style: italic;">An&aacute;lisis y Conclusiones sobre el Concepto Geof&iacute;sico &#8220;Tsunami Earthquakes&#8221; mediante Modelos Matem&aacute;ticos Simples</span>, desarrollado por el primer autor con el Apoyo a la Reincorporaci&oacute;n de Exbecarios PROMEP (Programa de Mejoramiento del Profesorado de la Secretar&iacute;a de Educaci&oacute;n P&uacute;blica de M&eacute;xico). El &#8220;M&oacute;dulo Sintetizador de Tsunamis&#8221; se desarroll&oacute; en el CICESE (Centro de Investigaci&oacute;n Cient&iacute;fica y de Educaci&oacute;n Superior de Ensenada) con el apoyo del Proyecto de Ciencia B&aacute;sica de CONACYT (Consejo Nacional de Ciencia y Tecnolog&iacute;a): <span style="font-style: italic;">Dise&ntilde;o de un Sistema Regional de Alerta de Tsunamis</span>, con n&uacute;mero de registro U51457-F.</span></font><br  style="font-family: verdana;"> <hr style="width: 100%; height: 2px;"><br style="font-family: verdana;"> <font style="font-weight: bold;" size="3"><span  style="font-family: verdana;">Referencias</span></font><br  style="font-family: verdana;">     <!-- ref --><br> <br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">1 Ewing, W.; Jardetzky, W. (1957) <span style="font-style: italic;">Elastic Waves in Layered Media</span>. McGraw Hill, New York.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932051&pid=S1409-2433201200010000900001&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    <!-- ref --><br> 2 Gonz&aacute;lez-Gonz&aacute;lez R. (2005) <span style="font-style: italic;">Hydroelastic Model on Tsunami Generation</span>. Ph.D. Thesis, Moscow State University, M.V. Lomonosov, Moscow, Russia.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932053&pid=S1409-2433201200010000900002&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    <!-- ref --><br> 3 Goto, C.; Ogawa, Y.; Shuto, N.; Imamura F. (1997) IUGG/IOC TIME <span style="font-style: italic;">Project: Numerical Method of Tsunami Simulation with the Leap-Frog Scheme</span>. Intergovernmental Oceanographic Commission of UNESCO, Manuals and Guides 35, Paris.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932055&pid=S1409-2433201200010000900003&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    <!-- ref --><br> 4 Gvozdev A.A.; Sekerzh Zen&#8217;kovich S.Ya.; Shingareva I.K. (2000) &#8220;Excitation of tsunami by a low-frequency nonstationary center of expansion&#8221;. <span  style="font-style: italic;">Izvestiya Physics of the Solid Earth</span>, Vol.36, No.1, 12&#8211;19.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932057&pid=S1409-2433201200010000900004&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    ]]></body>
<body><![CDATA[<!-- ref --><br> 5 Kanamori H.; Kikuchi M. (1993) &#8220;The 1992 Nicaragua earthquake: a slow tsunami earthquake associated with subducted sediments&#8221;. <span  style="font-style: italic;">Nature</span>, Vol. 361, 714&#8211;716.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932059&pid=S1409-2433201200010000900005&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    <!-- ref --><br> 6 Lamb, H. (1997) <span style="font-style: italic;">Hydrodynamics</span>. Cambridge University Press, Cambridge.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932061&pid=S1409-2433201200010000900006&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    <!-- ref --><br> 7 Mansinha, L.; Smylie D.E.(1971) &#8220;The displacement field of inclined faults&#8221;, <span style="font-style: italic;">Bulletin of the Seimological Society of America</span>, 61(5), 1433&#8211; 1440.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932063&pid=S1409-2433201200010000900007&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    <!-- ref --><br> 8 Pedlosky, J. (1979) <span style="font-style: italic;">Geophysical Fluid Dynamics</span>. Springer-Verlag, New York.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932065&pid=S1409-2433201200010000900008&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">     <!-- ref --><br> 9 Pod&#8221;yapol&#8217;skiy G.S. (1968)&#8220;Excitation of a long gravitational wave in the ocean from a seismic source in the crust&#8221;. <span style="font-style: italic;">Izvestiya Akademica Nauka. SSSR Fizika Zemli</span> 1, 7&#8211;24.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932067&pid=S1409-2433201200010000900009&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></span></font><br style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;">    ]]></body>
<body><![CDATA[<!-- ref --><br> 10 Zvolinskii N.V.; Nikitin I.S.; Sekerzh Zen&#8217;kovich S.Ya. (1991) &#8220;Excitation of tsunami waves and Rayleigh waves by a harmonic expansion center&#8221;. <span  style="font-style: italic;">Izvestiya Earth Physics</span>. Vol.23, No.2, 115&#8211;121.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=1932069&pid=S1409-2433201200010000900010&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --><br>     <br> <a name="correspondencia1"></a><a href="#correspondencia2">*</a>Correspondencia a: </span></font><font size="2"> <span style="font-family: verdana;">Rodrigo Gonz&aacute;lez Gonz&aacute;lez. </span></font><font size="2"><span  style="font-family: verdana;">Departamento de Matem&aacute;ticas, Universidad de Sonora. Hermosillo, Sonora, M&eacute;xico. E-Mail: <a href="mailto:rgonzlz@gauss.mat.uson.mx">rgonzlz@gauss.mat.uson.mx</a></span></font><br  style="font-family: verdana;"> <font size="2"> <span style="font-family: verdana;">Modesto Ortiz Figueroa. </span></font><font  size="2"><span style="font-family: verdana;">Departamento de Oceanograf&iacute;a F&iacute;sica, CICESE. Ensenada, Baja California, M&eacute;xico. E-Mail: <a href="mailto:ortizf@cicese.mx">ortizf@cicese.mx</a></span></font><br  style="font-family: verdana;"> <font size="2"> <span style="font-family: verdana;">Jos&eacute; Miguel Montoya Rodr&iacute;guez.</span></font><font size="2"><span  style="font-family: verdana;"> Divisi&oacute;n de Ingenier&iacute;a de Puertos y Costas, Instituto Mexicano del Transporte. Quer&eacute;taro, M&eacute;xico. E-Mail: <a  href="mailto:mmontoya@imt.mx">mmontoya@imt.mx</a>    <br>     <br> </span></font><font size="2"><span style="font-family: verdana;"><a  name="afiliacion1"></a><a href="#afiliacionh4">*</a>Departamento de Matem&aacute;ticas, Universidad de Sonora. Hermosillo, Sonora, M&eacute;xico. E-Mail: <a href="mailto:rgonzlz@gauss.mat.uson.mx">rgonzlz@gauss.mat.uson.mx</a></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;"><a name="afiliacion2"></a><a  href="#afiliacion5">&#8224;</a>Departamento de Oceanograf&iacute;a F&iacute;sica, CICESE. Ensenada, Baja California, M&eacute;xico. E-Mail: <a href="mailto:ortizf@cicese.mx">ortizf@cicese.mx</a></span></font><br  style="font-family: verdana;"> <font size="2"><span style="font-family: verdana;"><a name="afiliacion3"></a><a  href="#afiliacion6">&#8225;</a>Divisi&oacute;n de Ingenier&iacute;a de Puertos y Costas, Instituto Mexicano del Transporte. Quer&eacute;taro, M&eacute;xico. E-Mail: <a  href="mailto:mmontoya@imt.mx">mmontoya@imt.mx</a></span></font><br  style="font-family: verdana;">     <div style="text-align: center;"><font style="font-weight: bold;"  size="2"><span style="font-family: verdana;"></span></font> <hr style="width: 100%; height: 2px;"><font style="font-weight: bold;"  size="2"><span style="font-family: verdana;">Received: 13-Feb-2010; Revised: 28-Oct-2011; Accepted: 30-Nov-2011</span></font><br  style="font-family: verdana;"> </div> </div> </div>      ]]></body><back>
<ref-list>
<ref id="B1">
<label>1</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Ewing]]></surname>
<given-names><![CDATA[W]]></given-names>
</name>
<name>
<surname><![CDATA[Jardetzky]]></surname>
<given-names><![CDATA[W]]></given-names>
</name>
</person-group>
<source><![CDATA[Elastic Waves in Layered Media]]></source>
<year>1957</year>
<publisher-loc><![CDATA[^eNew York New York]]></publisher-loc>
<publisher-name><![CDATA[McGraw Hill]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B2">
<label>2</label><nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[González-González]]></surname>
<given-names><![CDATA[R]]></given-names>
</name>
</person-group>
<source><![CDATA[Hydroelastic Model on Tsunami Generation]]></source>
<year>2005</year>
</nlm-citation>
</ref>
<ref id="B3">
<label>3</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Goto]]></surname>
<given-names><![CDATA[C]]></given-names>
</name>
<name>
<surname><![CDATA[Ogawa]]></surname>
<given-names><![CDATA[Y]]></given-names>
</name>
<name>
<surname><![CDATA[Shuto]]></surname>
<given-names><![CDATA[N]]></given-names>
</name>
<name>
<surname><![CDATA[Imamura]]></surname>
<given-names><![CDATA[F]]></given-names>
</name>
</person-group>
<source><![CDATA[IUGG/IOC TIME Project: Numerical Method of Tsunami Simulation with the Leap-Frog Scheme]]></source>
<year>1997</year>
<publisher-loc><![CDATA[^eParis Paris]]></publisher-loc>
<publisher-name><![CDATA[Intergovernmental Oceanographic Commission of UNESCO]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B4">
<label>4</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Gvozdev]]></surname>
<given-names><![CDATA[A.A]]></given-names>
</name>
<name>
<surname><![CDATA[Sekerzh Zen&#8217;kovich]]></surname>
<given-names><![CDATA[S.Ya]]></given-names>
</name>
<name>
<surname><![CDATA[Shingareva]]></surname>
<given-names><![CDATA[I.K]]></given-names>
</name>
</person-group>
<article-title xml:lang="en"><![CDATA[Excitation of tsunami by a low-frequency nonstationary center of expansion]]></article-title>
<source><![CDATA[Izvestiya Physics of the Solid Earth]]></source>
<year>2000</year>
<volume>36</volume>
<numero>1</numero>
<issue>1</issue>
<page-range>12-19</page-range></nlm-citation>
</ref>
<ref id="B5">
<label>5</label><nlm-citation citation-type="">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Kanamori]]></surname>
<given-names><![CDATA[H]]></given-names>
</name>
<name>
<surname><![CDATA[Kikuchi]]></surname>
<given-names><![CDATA[M]]></given-names>
</name>
</person-group>
<article-title xml:lang="en"><![CDATA[The 1992 Nicaragua earthquake: a slow tsunami earthquake associated with subducted sediments]]></article-title>
<source><![CDATA[]]></source>
<year>1993</year>
<volume>361</volume>
<page-range>714-716</page-range></nlm-citation>
</ref>
<ref id="B6">
<label>6</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Lamb]]></surname>
<given-names><![CDATA[H]]></given-names>
</name>
</person-group>
<source><![CDATA[Hydrodynamics]]></source>
<year>1997</year>
<publisher-loc><![CDATA[^eCambridge Cambridge]]></publisher-loc>
<publisher-name><![CDATA[Cambridge University Press]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B7">
<label>7</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Mansinha]]></surname>
<given-names><![CDATA[L]]></given-names>
</name>
<name>
<surname><![CDATA[Smylie]]></surname>
<given-names><![CDATA[D.E]]></given-names>
</name>
</person-group>
<article-title xml:lang="en"><![CDATA[The displacement field of inclined faults]]></article-title>
<source><![CDATA[Bulletin of the Seimological Society of America]]></source>
<year>1971</year>
<volume>61</volume>
<numero>5</numero>
<issue>5</issue>
<page-range>1433- 1440</page-range></nlm-citation>
</ref>
<ref id="B8">
<label>8</label><nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Pedlosky]]></surname>
<given-names><![CDATA[J]]></given-names>
</name>
</person-group>
<source><![CDATA[Geophysical Fluid Dynamics]]></source>
<year>1979</year>
<publisher-loc><![CDATA[^eNew York New York]]></publisher-loc>
<publisher-name><![CDATA[Springer-Verlag]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B9">
<label>9</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Pod&#8221;yapol&#8217;skiy]]></surname>
<given-names><![CDATA[G.S]]></given-names>
</name>
</person-group>
<article-title xml:lang="en"><![CDATA[Excitation of a long gravitational wave in the ocean from a seismic source in the crust]]></article-title>
<source><![CDATA[Izvestiya Akademica Nauka]]></source>
<year>1968</year>
<volume>1</volume>
<page-range>7-24</page-range><publisher-name><![CDATA[SSSR Fizika Zemli]]></publisher-name>
</nlm-citation>
</ref>
<ref id="B10">
<label>10</label><nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Zvolinskii]]></surname>
<given-names><![CDATA[N.V]]></given-names>
</name>
<name>
<surname><![CDATA[Nikitin]]></surname>
<given-names><![CDATA[I.S]]></given-names>
</name>
<name>
<surname><![CDATA[Sekerzh Zen&#8217;kovich]]></surname>
<given-names><![CDATA[S.Ya]]></given-names>
</name>
</person-group>
<article-title xml:lang="en"><![CDATA[Excitation of tsunami waves and Rayleigh waves by a harmonic expansion center]]></article-title>
<source><![CDATA[Izvestiya Earth Physics]]></source>
<year>1991</year>
<volume>23</volume>
<numero>2</numero>
<issue>2</issue>
<page-range>115-121</page-range></nlm-citation>
</ref>
</ref-list>
</back>
</article>
