<?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>S1794-61902020000300345</article-id>
<article-id pub-id-type="doi">10.15446/esrj.v24n3.90315</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Calibration method of petroleum underground prospects based on high precision gravity and magnetic exploration]]></article-title>
<article-title xml:lang="es"><![CDATA[Método de calibración de prospectos de petróleo subterráneo con base en mediciones de gravedad de alta precisión y en exploración magnética]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zang]]></surname>
<given-names><![CDATA[Kai]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Wei]]></surname>
<given-names><![CDATA[Jiuchuan]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Yu]]></surname>
<given-names><![CDATA[Linsong]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Wan]]></surname>
<given-names><![CDATA[Fang]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hu]]></surname>
<given-names><![CDATA[Zunfang]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Li]]></surname>
<given-names><![CDATA[Yang]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Shandong University  ]]></institution>
<addr-line><![CDATA[Qingdao ]]></addr-line>
<country>China</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Shandong Institute of Geophysical  ]]></institution>
<addr-line><![CDATA[Jinan ]]></addr-line>
<country>China</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>09</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>09</month>
<year>2020</year>
</pub-date>
<volume>24</volume>
<numero>3</numero>
<fpage>345</fpage>
<lpage>355</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S1794-61902020000300345&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S1794-61902020000300345&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S1794-61902020000300345&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The high-precision calibration results of the petroleum underground layer are of great significance for oil production efficiency. This study uses the gravity magnetic model to retrieve the bedrock depth. The results of the basement structure and sedimentary rock distribution through the gravity and magnetic geology in the petroleum underground prospect of the Tongbai basin were also obtained. On this basis, the geological data, logging data, seismic data, and the Vertical Seismic Profile (VSP) data has been comprehensively used, as the layered calibration method was used to calibrate the petroleum underground layer. Considering the seismic datum and the core elevation in the area, the rock formation is divided by various logging curves. The average time difference and density of the divided rock layers are interpolated at equal depth intervals to obtain velocity sequences and density sequences at equal time intervals and finally realize time-depth conversion. When the drilling geological horizon is unified, the synthetic record of the seismic reflection layer is compared with the geological horizon to realize the horizon calibration of the seismic reflection layer. When the local stratification is not uniform, the seismic reflection layer is calibrated by tracking the seismic reflection layer, high-precision velocity analysis, and various synthetic records to verify the reliability of the geological horizon. The results show that the proposed method can accurately survey the geological conditions of the Tongbai basin. It detected 14 basement faults, and that the NW-trending and NE-trending faults controlled the basin, while the North-South faults controlled the later evolution of the basin. The method can be used for the horizon calibration of inclined wells, which is suitable not only for anisotropic media but also for formations with a less lateral variation of local formation lithology. Moreover, its usage is flexible, and it can be corrected by multiple speed data.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Debido a que los resultados de calibración de alta precisión de la capa subterránea de petróleo son de gran importancia para la eficiencia en la producción de petróleo, este estudio usa la investigación sobre el método de calibración de la capa subterránea de petróleo con base en la gravedad de alta precisión y la exploración magnética. El modelo magnético de gravedad se utilizó para medir la profundidad de la roca madre. Además se obtuvieron los resultados de la estructura del basamento y la distribución de rocas sedimentarias a través de la gravedad y la geología magnética en un prospecto de petróleo subterráneo en la cuenca Tongbai. Sobre esta base, los datos geológicos, los datos de registro, los datos sísmicos y los datos del Perfil Sísmico Vertical (VSP) se usaron de manera integral, y el método de calibración en capas se usó para calibrar la capa subterránea de petróleo de la cuenca Tongbai. De acuerdo con el dato sísmico y con la elevación del núcleo en el área, la formación rocosa se dividió en varias curvas de registro. La diferencia de tiempo promedio y la densidad de las capas de roca divididas se interpolaron a intervalos de profundidad iguales para obtener secuencias de velocidad y secuencias de densidad a intervalos de tiempo iguales, y finalmente realizar la conversión de profundidad de tiempo. Cuando el horizonte geológico de perforación se unifica, el registro sintético de la capa de reflexión sísmica se compara con el horizonte geológico para realizar la calibración del horizonte de la capa de reflexión sísmica. Cuando la estratificación local no es uniforme, la capa de reflexión sísmica se calibra con la capa de reflexión sísmica, el análisis de velocidad de alta precisión y varios registros sintéticos para verificar la fiabilidad del horizonte geológico. Los resultados muestran que el método propuesto puede estudiar con precisión las condiciones geológicas de la cuenca Tongbai. Este método detectó 14 fallas en el basamento, y también que las fallas de tendencia NW y NE controlaron la cuenca, mientras que las fallas norte-sur controlaron la evolución posterior de la cuenca. El método puede usarse para la calibración del horizonte de pozos inclinados, que es adecuado no solo para medios anisotrópicos, sino también para formaciones con menor variación lateral de la litología de formación local. Además, su uso es flexible y puede corregirse con múltiples datos de velocidad.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[high precision gravity and magnetic exploration]]></kwd>
<kwd lng="en"><![CDATA[petroleum]]></kwd>
<kwd lng="en"><![CDATA[underground layer]]></kwd>
<kwd lng="en"><![CDATA[layer calibration]]></kwd>
<kwd lng="en"><![CDATA[bedrock depth]]></kwd>
<kwd lng="es"><![CDATA[Alta precisión de gravedad]]></kwd>
<kwd lng="es"><![CDATA[exploración magnética]]></kwd>
<kwd lng="es"><![CDATA[petróleo]]></kwd>
<kwd lng="es"><![CDATA[capa subterránea]]></kwd>
<kwd lng="es"><![CDATA[calibración de capa]]></kwd>
<kwd lng="es"><![CDATA[profundidad de la roca madre]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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