<?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>2026-07-23T00:55:56Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/12100" metadataPrefix="qdc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/12100</identifier><datestamp>2025-09-15T12:47:54Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><qdc:qualifieddc xmlns:qdc="http://dspace.org/qualifieddc/" xmlns:dc="http://purl.org/dc/elements/1.1/" 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://purl.org/dc/elements/1.1/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dc.xsd http://purl.org/dc/terms/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dcterms.xsd http://dspace.org/qualifieddc/ http://www.ukoln.ac.uk/metadata/dcmi/xmlschema/qualifieddc.xsd">
   <dc:title>Epitactic Overgrowths of Calcite (CaCO3) on Anhydrite (CaSO4) Cleavage Surfaces</dc:title>
   <dc:creator>Cuesta Mayorga, Iris</dc:creator>
   <dc:creator>Astilleros García-Monge, José Manuel</dc:creator>
   <dc:creator>Fernández Díaz, María Lourdes</dc:creator>
   <dc:creator>Morales, Juan</dc:creator>
   <dc:creator>Prieto Rubio, Manuel</dc:creator>
   <dc:creator>Roncal-Herrero, Teresa</dc:creator>
   <dc:creator>Benning, Liane G.</dc:creator>
   <dcterms:abstract>We investigate the crystallographic relationships between calcite crystals overgrown on the (100), (010), and (001) anhydrite cleavage surfaces, as a result of the interaction between anhydrite surfaces with carbonate-rich aqueous solutions. This interaction always leads to oriented nucleation and growth of calcite crystals, characterized by a parallelism between the calcite {1014} faces and the corresponding anhydrite cleavage surface.</dcterms:abstract>
   <dcterms:dateAccepted>2023-06-17T12:27:21Z</dcterms:dateAccepted>
   <dcterms:available>2023-06-17T12:27:21Z</dcterms:available>
   <dcterms:created>2023-06-17T12:27:21Z</dcterms:created>
   <dcterms:issued>2018</dcterms:issued>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/12100</dc:identifier>
   <dc:identifier>1528-7483</dc:identifier>
   <dc:identifier>10.1021/acs.cgd.7b01610</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>CGL2013-47988-C2-1-P</dc:relation>
   <dc:relation>CGL2016-77138- C2-1-P. I.</dc:relation>
   <dc:rights>restricted access</dc:rights>
   <dc:publisher>American Chemical Society</dc:publisher>
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