<?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>2301-1513</journal-id>
<journal-title><![CDATA[Anales de Investigación en Arquitectura]]></journal-title>
<abbrev-journal-title><![CDATA[An. Investig. Arquit.]]></abbrev-journal-title>
<issn>2301-1513</issn>
<publisher>
<publisher-name><![CDATA[Universidad ORT Uruguay]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2301-15132025000201202</article-id>
<article-id pub-id-type="doi">10.18861/ania.2025.15.2.3972</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Iglesia de la Compañía de Jesús de Quito, historia de sus elementos constructivos]]></article-title>
<article-title xml:lang="en"><![CDATA[Church of the Company of Jesus of Quito, history of its construction elements]]></article-title>
<article-title xml:lang="pt"><![CDATA[Igreja da Companhia de Jesus de Quito, história de seus elementos construtivos]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lara Calderón]]></surname>
<given-names><![CDATA[Marco Lenin]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Internacional del Ecuador  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Ecuador</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<volume>15</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.edu.uy/scielo.php?script=sci_arttext&amp;pid=S2301-15132025000201202&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.edu.uy/scielo.php?script=sci_abstract&amp;pid=S2301-15132025000201202&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.edu.uy/scielo.php?script=sci_pdf&amp;pid=S2301-15132025000201202&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La iglesia de la Compañía de Jesús de Quito, construida entre 1605-1765, es uno de los ejemplos más notables de la arquitectura religiosa barroca latinoamericana, lugar de culto y exhibición de arte religioso de la época virreinal. En los 160 años se identifican tres fases constructivas y para 1765 la fachada de piedra tuvo un recubrimiento de mortero de cal que imita al mármol, conocido como "jaspe". El objetivo de esta investigación es establecer su composición para contribuir con la comprensión de la cronología constructiva del templo; se examinaron un total de 17 muestras de revestimiento, 14 corresponden a morteros de revestimiento del interior del templo y 3 muestras corresponden a la fachada de piedra superficial, extraídas con los protocolos y normas menos invasivas sugeridas por el equipo de investigación. Las muestras incluyen estudios de microscopía estereoscópica que se complementaron con caracterización de minerales y análisis cuantitativo por difracción de rayos X; así como microscopía óptica de luz polarizada y microscopía electrónica de barrido con microanálisis, entre otros. Los resultados de laboratorio permitieron demostrar la presencia de morteros de cal y yeso, y morteros de yeso con agregado carbonatado, dichos elementos tienen composición volcánica mineralógica y volcánicos metamórficos, estos permitieron corroborarlos dentro de las etapas constructivas registradas en la iglesia.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Church of the Company of Jesus in Quito, built between 1605-1765, is one of the most notable examples of Latin American Baroque religious architecture, a place of worship and exhibition of religious art of the viceregal era. In 160 years, three construction phases can be identified and by 1765 the stone facade had a lime mortar coating that mimics marble, known as 'jasper'. The objective of this research is to establish its composition to contribute to the understanding of the constructive chronology of the temple; A total of 17 coating samples were examined, 14 correspond to coating mortars from the interior of the temple and 3 samples correspond to the surface stone façade, extracted with the protocols and less invasive standards suggested by the research team. The samples include stereoscopic microscopy studies that were complemented with mineral characterization and quantitative analysis by X-ray diffraction, as well as polarized light optical microscopy and scanning electron microscopy with microanalysis, among others. Laboratory results demonstrated the presence of lime and gypsum mortars, and carbonated aggregate gypsum mortars, these elements have a volcanic mineralogical and metamorphic volcanic composition, which allowed us to corroborate them within the construction stages recorded in the church.]]></p></abstract>
<abstract abstract-type="short" xml:lang="pt"><p><![CDATA[Resumo A igreja da Compañía de Jesús em Quito, construída entre 1605-1765, é um dos exemplos mais notáveis da arquitetura religiosa barroca latino-americana, local de culto e exposição de arte religiosa da época vice-real. Ao longo dos 160 anos, foram identificadas três fases de construção e, em 1765, a fachada de pedra tinha um revestimento de argamassa de cal que imita o mármore, conhecido como &#8220;jaspe&#8221;. O objetivo desta investigação é estabelecer a sua composição de modo a contribuir para a compreensão da cronologia construtiva do templo; foram examinadas 17 amostras de revestimento, 14 correspondentes a argamassas de revestimento do interior do templo e 3 amostras correspondentes à fachada de pedra superficial, extraídas com os protocolos e normas menos invasivos sugeridos pela equipa de investigação, As amostras incluem estudos de estereomicroscopia que foram complementados com caraterização mineral e análise quantitativa por difração de raios X; bem como microscopia ótica de luz polarizada e microscopia eletrónica de varrimento com microanálise, entre outros. Os resultados laboratoriais demonstraram a presença de argamassas de cal e gesso, e argamassas de gesso com agregado carbonatado, elementos de composição mineralógica vulcânica e vulcânica metamórfica, o que os corroborou nas fases de construção registadas na igreja.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Morteros de cal]]></kwd>
<kwd lng="es"><![CDATA[Morteros de yeso]]></kwd>
<kwd lng="es"><![CDATA[Andesita]]></kwd>
<kwd lng="es"><![CDATA[Historia de la construcción]]></kwd>
<kwd lng="es"><![CDATA[Quito Patrimonio cultural]]></kwd>
<kwd lng="es"><![CDATA[Iglesia de la Compañía de Jesús en Quito]]></kwd>
<kwd lng="en"><![CDATA[Lime mortars]]></kwd>
<kwd lng="en"><![CDATA[Gypsum mortars]]></kwd>
<kwd lng="en"><![CDATA[Andesite]]></kwd>
<kwd lng="en"><![CDATA[History of the construction]]></kwd>
<kwd lng="en"><![CDATA[Quito cultural heritage]]></kwd>
<kwd lng="en"><![CDATA[Church of the company of Jesus of Quito]]></kwd>
<kwd lng="pt"><![CDATA[Argamassas de cal]]></kwd>
<kwd lng="pt"><![CDATA[Argamassas de gesso]]></kwd>
<kwd lng="pt"><![CDATA[Andesite]]></kwd>
<kwd lng="pt"><![CDATA[História da construção]]></kwd>
<kwd lng="pt"><![CDATA[Património cultural de Quito]]></kwd>
<kwd lng="pt"><![CDATA[Igreja da companhia de Jesus de Quito]]></kwd>
</kwd-group>
</article-meta>
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