<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-06-29T01:17:02Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/124229" metadataPrefix="marc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/124229</identifier><datestamp>2025-09-24T12:38:52Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><record xmlns="http://www.loc.gov/MARC21/slim" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd">
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      <subfield code="a">García Rivas, Javier</subfield>
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      <subfield code="a">Dias, Maria Isabel</subfield>
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      <subfield code="a">Paiva, Isabel</subfield>
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      <subfield code="a">Fernandes, Paula G.</subfield>
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      <subfield code="a">Marques, Rosa</subfield>
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      <subfield code="a">García Romero, Emilia</subfield>
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      <subfield code="a">Suárez, Mercedes</subfield>
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      <subfield code="c">2025-08-07</subfield>
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      <subfield code="a">This work aims to perform a detailed mineralogical, crystal-chemical, and geochemical characterization of bentonites from the Benavila outcrop, the largest known deposit of bentonites in continental Portugal. Bulk samples and different size fractions were characterized through X-Ray Diffraction (XRD). Structural formulae of the smectites were fitted from point analyses acquired by analytical electron microscopy (AEM) with transmission electron microscopy (TEM). Smectites are the major component with variable amounts of calcite and minor amounts of quartz, feldspar, illite, and chlorite. Occasionally, amphiboles and dolomite have also been identified. The high content of carbonates in different parts of the sampling area is related to the circulation of carbonate-rich fluids. The smectites present high-layer charge, are intermediate terms of the montmorillonite–beidellite series, and also show an intermediate cisvacant–transvacant configuration. Major and trace elements concentrations were determined by ICP-MS. The geochemical analysis of the samples indicates an enrichment in SiO2 and Al2O3 and a depletion of the more clayey materials in REE, HFSE, and Y, among others. The calculation of the PIA and CIA alteration indices, along with other parameters observed, shows the possible alteration pathways of the Benavila deposit. Research to evaluate the ability of these bentonites to be used as engineering barrier systems (EBS) and sealing materials for radioactive waste repositories is ongoing.</subfield>
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      <subfield code="a">García-Rivas, J., Dias, M. I., Paiva, I., Fernandes, P. G., Marques, R., García-Romero, E., &amp; Suárez, M. (2025). Mineralogical and geochemical characterization of the benavila (Portugal) bentonites. Minerals, 15(8), 836. https://doi.org/10.3390/min15080836</subfield>
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      <subfield code="a">10.3390/min15080836</subfield>
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      <subfield code="a">https://hdl.handle.net/20.500.14352/124229</subfield>
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      <subfield code="a">2075-163X</subfield>
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      <subfield code="a">https://doi.org/10.3390/min15080836</subfield>
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      <subfield code="a">https://openpolicyfinder.jisc.ac.uk/id/publication/18600</subfield>
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   <datafield ind2="0" ind1="0" tag="245">
      <subfield code="a">Mineralogical and geochemical characterization of the Benavila (Portugal) bentonites</subfield>
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