<?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>2026-04-17T15:51:19Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2445/183814" metadataPrefix="oai_dc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2445/183814</identifier><datestamp>2025-12-05T14:28:34Z</datestamp><setSpec>com_2072_1057</setSpec><setSpec>col_2072_478917</setSpec><setSpec>col_2072_478923</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <dc:title>Talc- and serpentine-like 'garnierites' from Falcondo Ni-laterite deposit (Dominican Republic): a HRTEM approach</dc:title>
   <dc:creator>Villanova de Benavent, Cristina</dc:creator>
   <dc:creator>Nieto, Fernando</dc:creator>
   <dc:creator>Proenza Fernández, Joaquín Antonio</dc:creator>
   <dc:creator>Galí Medina, Salvador, 1949-</dc:creator>
   <dc:subject>Jaciments minerals</dc:subject>
   <dc:subject>Talc</dc:subject>
   <dc:subject>República Dominicana</dc:subject>
   <dc:subject>Mineral deposits</dc:subject>
   <dc:subject>Talc</dc:subject>
   <dc:subject>Dominican Republic</dc:subject>
   <dc:description>"Garnierites" represent significant Ni ore minerals in the lower horizons of many Ni-laterite deposits worldwide (e.g. Freyssinet et al., 2005). They consist of a green, fine-grained mixture of hydrous i-bearing magnesium phyllosilicates, including serpentine, talc, sepiolite, smectite and chlorite (e.g. Brindley and Hang, 1973; Springer, 1974; Brindley et al., 1979). Thus, "garnierite" is a general descriptive term and is not recognized as a mineral species by the IMA Commission on New Mineral and Mineral Names (CNMMN). For this reason, "garnierites" have been classified as "serpentine-", "talc-" and "clay-like garnierites", respectively (e.g. Brindley and Maksimovic, 1974).</dc:description>
   <dc:date>2022-03-07T08:41:58Z</dc:date>
   <dc:date>2022-03-07T08:41:58Z</dc:date>
   <dc:date>2011</dc:date>
   <dc:date>2022-03-07T08:41:59Z</dc:date>
   <dc:type>info:eu-repo/semantics/article</dc:type>
   <dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
   <dc:identifier>1885-7264</dc:identifier>
   <dc:identifier>https://hdl.handle.net/2445/183814</dc:identifier>
   <dc:identifier>616348</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>Reproducció del document publicat a: http://www.semineral.es/websem/PdfServlet?mod=archivos&amp;subMod=publicaciones&amp;archivo=Macla15_197.pdf</dc:relation>
   <dc:relation>MACLA. Revista de la Sociedad Española de Mineralogía, 2011, vol. 15, p. 197-198</dc:relation>
   <dc:rights>(c) Villanova de Benavent, Cristina et al., 2011</dc:rights>
   <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
   <dc:format>2 p.</dc:format>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Sociedad Española de Mineralogía</dc:publisher>
   <dc:source>Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)</dc:source>
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