<?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>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692016000100017</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Tectonic Interpretation of Topographic Lineaments in the Seacoast Region of New Hampshire, U. S. A.]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Escamilla-Casas]]></surname>
<given-names><![CDATA[José Cruz]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Schulz]]></surname>
<given-names><![CDATA[Jeffrey E.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma del Estado de Hidalgo Área Académica de Ciencias de la Tierra y Materiales ]]></institution>
<addr-line><![CDATA[ Hidalgo]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Weston Solutions, Inc.  ]]></institution>
<addr-line><![CDATA[Anchorage AK]]></addr-line>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2016</year>
</pub-date>
<volume>55</volume>
<numero>1</numero>
<fpage>17</fpage>
<lpage>37</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692016000100017&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692016000100017&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692016000100017&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: The identification of topographic lineaments on Digital Elevation Models, high-resolution bathymetric soundings, and an ordinary Kriging prediction map provide the basis for refinement of the traces of known fault zones associated with the Norumbega Fault System in the seacoast region of New Hampshire. On the present topography, simple Euler poles analysis suggests the association of the course of the Piscataqua and the Cocheco rivers with the mechanics of emplacement of the Mesozoic Agamenticus Complex. Topographic profiles, bathymetric soundings, structural analysis of brittle structures, and an ordinary Kriging prediction map of the bedrock topography support the presence of a sub-circular structure that is being interpreted as related to a subsurface plutonic body. An extensional regime model is being presented to illustrate the possible tectonic evolution of Great Bay tidal estuary.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: La identificación de lineamientos topográficos en modelos digitales de elevación, en sondeos batimétricos de alta resolución y en un mapa predictivo de la topografía del lecho rocoso, permite precisar las trazas de fallas asociadas al Sistema Norumbega, en la costa de New Hampshire. El análisis de polos simples de Euler sugiere que la formación del cauce de los ríos Cocheco y Piscataqua muy probablemente estuvo relacionada con los mecanismos de emplazamiento del Complejo Agamenticus del Mesozoico. Los análisis en perfiles topográficos, sondeos batimétricos, topografía del lecho rocoso y el análisis estructural de la deformación frágil confirman la presencia de un cuerpo plutónico sub-circular no expuesto. Finalmente, presentamos un modelo que explica, tentativamente, la evolución tectónica del estuario Great Bay.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Great Bay estuary]]></kwd>
<kwd lng="en"><![CDATA[Rye formation]]></kwd>
<kwd lng="en"><![CDATA[Merrimack group]]></kwd>
<kwd lng="en"><![CDATA[Norumbega fault system]]></kwd>
<kwd lng="en"><![CDATA[Kriging analysis]]></kwd>
<kwd lng="es"><![CDATA[Estuario de Great Bay]]></kwd>
<kwd lng="es"><![CDATA[formación Rye]]></kwd>
<kwd lng="es"><![CDATA[grupo Merrimack]]></kwd>
<kwd lng="es"><![CDATA[sistema de fallas Norumbega]]></kwd>
<kwd lng="es"><![CDATA[análisis Kriging]]></kwd>
</kwd-group>
</article-meta>
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<name>
<surname><![CDATA[Hussey]]></surname>
<given-names><![CDATA[A.M.]]></given-names>
</name>
<name>
<surname><![CDATA[Fanning]]></surname>
<given-names><![CDATA[C.M.]]></given-names>
</name>
</person-group>
<source><![CDATA[American Journal of Science]]></source>
<year>2007</year>
<volume>307</volume>
<page-range>119-67</page-range></nlm-citation>
</ref>
</ref-list>
</back>
</article>
