<?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>1794-6190</journal-id>
<journal-title><![CDATA[Earth Sciences Research Journal]]></journal-title>
<abbrev-journal-title><![CDATA[Earth Sci. Res. J.]]></abbrev-journal-title>
<issn>1794-6190</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional de Colombia]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1794-61902019000400283</article-id>
<article-id pub-id-type="doi">10.15446/esrj.v23n4.84000</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Basic Characteristics and Evolution of Geological Structures in the Eastern Margin of the Qinghai-Tibet Plateau]]></article-title>
<article-title xml:lang="es"><![CDATA[Características básicas y evolución de las estructuras geológicas en el margen oriental de la meseta Qinghai-Tíbet]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Deng]]></surname>
<given-names><![CDATA[Dejie]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Wang]]></surname>
<given-names><![CDATA[Changliu]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Peng]]></surname>
<given-names><![CDATA[Peihao]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Chengdu University of Technology  ]]></institution>
<addr-line><![CDATA[Chengdu ]]></addr-line>
<country>China</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Southwest Minzu University  ]]></institution>
<addr-line><![CDATA[Chengdu ]]></addr-line>
<country>China</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Chengdu University of Technology  ]]></institution>
<addr-line><![CDATA[Chengdu ]]></addr-line>
<country>China</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<volume>23</volume>
<numero>4</numero>
<fpage>283</fpage>
<lpage>291</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S1794-61902019000400283&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S1794-61902019000400283&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S1794-61902019000400283&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Based on field geological survey and stratigraphic profile survey in the eastern margin of the Qinghai-Tibet Plateau, the basic characteristics and evolution of geological structure in the eastern margin of the Qinghai-Tibet Plateau are studied. The Dongyuan area of the Qinghai-Tibet Plateau is divided into the late Cenozoic period and the current period. During the Late Cenozoic, the Pliocene Xigeda lacustrine deposits develops from 4.2 MaBP to 2.6 MaBP, with 9 cold-warm climate change stages. There are 4.3 MaBP old glacial period in this area, and 5 extreme paleoclimate events in Quaternary. At present, the horizontal movement intensity and mode of different tectonic zones are determined by the northward extrusion, eastward extrusion and rotation around the eastern tectonic junction in the study area, and the stages of the movement state changing with time are related to the gestation and occurrence of extra-large earthquakes. At present, the three-dimensional crustal movement shows that the tectonic activity differentiation of mountain and basin, which is related to tectonic dynamic environment and deep material activity, is related to the compression, shortening and uplift of plateau mountain and the extension and subsidence of basin, reflecting the inheritance of neotectonic activity. Through practical analysis, it is found that the eastern margin of the Qinghai-Tibet Plateau is composed of Minshan fault block and Longmenshan structural belt. The left-lateral dislocation of Minjiang fault is roughly the same as the vertical dislocation. In Longmenshan tectonic belt, the right-lateral dislocation of Maowen-Wenchuan fault, Beichuan-Yingxiu fault and other main faults is the same as the vertical dislocation.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En este trabajo se estudian las características básicas y la evolución de la estructura geológica en el margen oriental de la meseta Qinghai-Tíbet con base en el análisis geológico de campo y el estudio del perfil estratigráfico de la zona de estudio. El área de Dongyuan de la meseta Qinghai-Tíbet se divide en el período Cenozoico tardío y el período actual. Durante el Cenozoico Tardío, los depósitos lacustres del Plioceno Xigeda se desarrollaron de 4.2 MaBP a 2.6 MaBP, con 9 etapas de cambio climático frío-cálido. Hay 4.3 MaBP viejos períodos glaciales en esta área, y cinco eventos paleoclimáticos extremos en el Cuaternario. En la actualidad, la intensidad del movimiento horizontal y el modo de las diferentes zonas tectónicas están determinados por la extrusión hacia el norte, la extrusión hacia el este y la rotación alrededor de la unión tectónica oriental en el área de estudio, y las etapas del cambio del estado del movimiento con el tiempo están relacionadas con la gestación y ocurrencia de terremotos extragrandes. En la actualidad, el movimiento cortical tridimensional muestra que la diferenciación de la actividad tectónica de la montaña y la cuenca, que está relacionada con el entorno dinámico tectónico y la actividad del material profundo, está relacionada con la compresión, el acortamiento y la elevación de la meseta de montaña y la extensión y hundimiento de cuenca, que refleja la herencia de la actividad neotectónica. A través del análisis práctico, se descubre que el margen oriental de la meseta Qinghai-Tíbet está compuesto por el bloque de falla Minshan y el cinturón estructural Longmenshan. La dislocación lateral izquierda de la falla de Minjiang es aproximadamente la misma que la dislocación vertical. En el cinturón tectónico de Longmenshan, la dislocación lateral derecha de la falla de Maowen-Wenchuan, la falla de Beichuan-Yingxiu y otras fallas principales es la misma que la dislocación vertical.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Qinghai-Tibet Plateau]]></kwd>
<kwd lng="en"><![CDATA[Eastern margin area]]></kwd>
<kwd lng="en"><![CDATA[Geological structure]]></kwd>
<kwd lng="en"><![CDATA[Basic characteristics]]></kwd>
<kwd lng="en"><![CDATA[Evolution research]]></kwd>
<kwd lng="en"><![CDATA[Crustal movement]]></kwd>
<kwd lng="es"><![CDATA[meseta Qinghai-Tibet]]></kwd>
<kwd lng="es"><![CDATA[Area del margen oriental]]></kwd>
<kwd lng="es"><![CDATA[Estructura geológica]]></kwd>
<kwd lng="es"><![CDATA[Características básicas]]></kwd>
<kwd lng="es"><![CDATA[Investigación de la evolución]]></kwd>
<kwd lng="es"><![CDATA[Movimiento de la corteza]]></kwd>
</kwd-group>
</article-meta>
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