<?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>2026-06-30T20:34:23Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/58272" metadataPrefix="oai_dc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/58272</identifier><datestamp>2023-08-25T15:45:08Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</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>Edificios volcánicos en la Serie I de Fuerteventura:
Rasgos generales del edificio central</dc:title>
   <dc:creator>Ancochea Soto, Eumenio</dc:creator>
   <dc:creator>Cubas , C.R.</dc:creator>
   <dc:creator>Hernán , F.</dc:creator>
   <dc:creator>Brandle, J.L.</dc:creator>
   <dc:subject>552.3(460.413)</dc:subject>
   <dc:subject>Volcanic edifices</dc:subject>
   <dc:subject>Old basaltic Series</dc:subject>
   <dc:subject>Fuerteventura</dc:subject>
   <dc:subject>Canary Island.</dc:subject>
   <dc:subject>Petrología</dc:subject>
   <dc:description>The Old Basaltic Series in Fuerteventura is formed by three main edifices: Northern, Central
and Southern (or jandíaJ Edifices.
The Central Edifice, a shield volcano, extends from El jable towards Valles Ortega area forming
a semicircular shape around a large adjacet basin. The edifice is built up by dipping outwards thick
basaltic flows piles in which pyroclastic are scarce. Three different subseries, can be distinguished
within these piles: Lower, Medium and Upper Series, all separated by unconformities. A fourth active
episode, the Late Series, filled the inner basin, and was clearly emitted after a large tectonic
graben took place.</dc:description>
   <dc:description>Depto. de Mineralogía y Petrología</dc:description>
   <dc:description>Fac. de Ciencias Geológicas</dc:description>
   <dc:description>TRUE</dc:description>
   <dc:description>pub</dc:description>
   <dc:date>2023-06-20T17:27:57Z</dc:date>
   <dc:date>2023-06-20T17:27:57Z</dc:date>
   <dc:date>1991</dc:date>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/58272</dc:identifier>
   <dc:identifier>0213-683X</dc:identifier>
   <dc:language>spa</dc:language>
   <dc:rights>open access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Sociedad Geológica de España</dc:publisher>
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