<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222022000200109</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2022v74n2a240322</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Microbiostratigraphy, microfacies analysis and lateral basin evolution of Lower Cretaceous deposits in the south of Kerman region, SE Iran]]></article-title>
<article-title xml:lang="es"><![CDATA[Microbioestratigrafía, análisis de microfacies y evolución lateral de la cuenca de los depósitos del Cretácico Inferior en la región sur de Kerman, SE Irán]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hassani]]></surname>
<given-names><![CDATA[Mohammad Javad]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Graduate University of Advanced Technology Institute of Science and High Technology and Environmental Sciences Department of Ecology]]></institution>
<addr-line><![CDATA[Kerman ]]></addr-line>
<country>Iran</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>74</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222022000200109&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222022000200109&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222022000200109&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Detailed microbiostratigraphy and basin evolution of the Lower Cretaceous deposits in the Rayen area, south of Kerman Region, SE Iran are investigated for the first time in two sections. The section no. 1 is 324.6m in thickness and comprises five lithostratigraphic units. The section no. 2 is 218 m in thickness and includes three lithostratigraphic units. The identified fauna and flora include 41 benthic foraminifera and 11 calcareous algae species. The identified assemblage indicates that the marine strata in both sections were deposited during the Barremian to Albian. The microfacies analyses carried out on 22 carbonate and 2 clastic microfacies indicate that the deposits in the section no. 1 were deposited on a homoclinal carbonate ramp, whereas in the section no. 2 they were deposited on a rimmed carbonate shelf. Generally, the Cretaceous deposit in the two studied sections represent different sedimentary models and fossil content indicating different basin evolution histories. The paleogeographic setting of the studied area on the south eastern margin of the Central-East Iranian Microcontinent and the active tectonic history during the Mesozoic suggest that the syndepositional tectonism influenced the basement&#8217;s morphology and resulted in changes in the fossil diversity and sedimentary nature of adjacent sedimentary basins.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La microbioestratigrafía detallada y la evolución de la cuenca de los depósitos del Cretácico Inferior en el área de Rayen, al sur de la región de Kerman, sureste de Irán, se investigan por primera vez en dos secciones. La sección núm. 1 tiene 324.6 m de espesor y comprende cinco unidades litoestratigráficas. La sección núm. 2 tiene 218 m de espesor e incluye tres unidades litoestratigráficas. La fauna y flora identificada incluye 41 foraminíferos bentónicos y 11 especies de algas calcáreas. El conjunto identificado indica que los estratos marinos en ambas secciones fueron depositados durante el Barremiense al Albiense. Los análisis de microfacies realizados en 22 microfacies carbonatadas y 2 clásticas indican que los depósitos en la sección no. 1 se depositaron en una rampa de carbonato homoclinal, mientras que en la sección no. 2 se depositaron en una plataforma carbonatada con borde. En general, el depósito del Cretácico en las dos secciones estudiadas representan diferentes modelos sedimentarios y contenido fósil que indican diferentes historias de evolución de la cuenca. El marco paleogeográfico del área estudiada en el margen suroriental del microcontinente iraní centro-oriental y la historia tectónica activa durante el Mesozoico sugieren que el tectonismo sindeposicional influyó en la morfología del basamento y resultó en cambios en la diversidad fósil y la naturaleza sedimentaria de sedimentos adyacentes. cuencas.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Lower Cretaceous]]></kwd>
<kwd lng="en"><![CDATA[CEIM]]></kwd>
<kwd lng="en"><![CDATA[basin evolution]]></kwd>
<kwd lng="en"><![CDATA[Kerman]]></kwd>
<kwd lng="en"><![CDATA[Rayen]]></kwd>
<kwd lng="es"><![CDATA[Cretácico Inferior]]></kwd>
<kwd lng="es"><![CDATA[CEIM]]></kwd>
<kwd lng="es"><![CDATA[evolución de cuencas]]></kwd>
<kwd lng="es"><![CDATA[Kerman]]></kwd>
<kwd lng="es"><![CDATA[Rayen]]></kwd>
</kwd-group>
</article-meta>
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