<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
    <record>
        <controlfield tag="001">58756</controlfield>
        <controlfield tag="005">20170831220647.0</controlfield>
        <datafield tag="037" ind1=" " ind2=" ">
            <subfield code="a">TAZ-TFM-2016-230</subfield>
        </datafield>
        <datafield tag="041" ind1=" " ind2=" ">
            <subfield code="a">spa</subfield>
        </datafield>
        <datafield tag="100" ind1="1" ind2=" ">
            <subfield code="a">Laita Florian, Elisa</subfield>
        </datafield>
        <datafield tag="242" ind1="0" ind2="0">
            <subfield code="a">Mineral transformations in aluminium-rich clays with firing and their relation with significant properties</subfield>
        </datafield>
        <datafield tag="245" ind1="0" ind2="0">
            <subfield code="a">Transformaciones minerales durante los procesos de cocción de arcillas alumínicas y su relación con propiedades físicas de interés</subfield>
        </datafield>
        <datafield tag="260" ind1=" " ind2=" ">
            <subfield code="a">Zaragoza</subfield>
            <subfield code="b">Universidad de Zaragoza</subfield>
            <subfield code="c">2016</subfield>
        </datafield>
        <datafield tag="506" ind1=" " ind2=" ">
            <subfield code="a">by-nc-sa</subfield>
            <subfield code="b">Creative Commons</subfield>
            <subfield code="c">3.0</subfield>
            <subfield code="u">http://creativecommons.org/licenses/by-nc-sa/3.0/</subfield>
        </datafield>
        <datafield tag="520" ind1=" " ind2=" ">
            <subfield code="a">Mineralogical and textural transformations and changes in physical properties of three shales fired from 800 to 1300ºC have been studied. Initially these samples were formed by variable proportions of illite, pyrophyllite, orthoclase, quartz, kaolinite, mixed layers I/S and organic matter. Raw and fired samples were analysed by X-ray diffraction, transmitted light microscopy, field emission scanning electron microscopy and transmission electron microscopy. Kaolinite, mixed layers I/S and organic matter were destabilized at temperatures below 800°C indicating that they are the least stable phases to the firing process. Illite, pyrophyllite and orthoclase remain until 1000ºC and they show a larger stability field during the ceramic process than in natural environments. Quartz remains during all the firing process, although it is partly replaced by vitreous material. When temperature increases, hematite and mullite crystallize and the vitrification starts from 1000ºC. This vitreous phase is the precursor of mullite. Changes in colour (grey-orange-brown) are due to the loss of organic matter, to the formation of hematite and its subsequent destabilization. Variations in linear contraction, density, total porosity and in average pore size are related to the destabilization of the different phases, the progress of vitrification and the crystallization of mullite.</subfield>
        </datafield>
        <datafield tag="521" ind1=" " ind2=" ">
            <subfield code="a">Máster Universitario en Geología: Técnicas y aplicaciones</subfield>
        </datafield>
        <datafield tag="540" ind1=" " ind2=" ">
            <subfield code="a">Derechos regulados por licencia Creative Commons</subfield>
        </datafield>
        <datafield tag="700" ind1=" " ind2=" ">
            <subfield code="a">Bauluz Lázaro, Blanca</subfield>
            <subfield code="e">dir.</subfield>
        </datafield>
        <datafield tag="710" ind1="2" ind2=" ">
            <subfield code="a">Universidad de Zaragoza</subfield>
            <subfield code="b">Ciencias de la Tierra</subfield>
            <subfield code="c">Cristalografía y Mineralogía</subfield>
        </datafield>
        <datafield tag="856" ind1="0" ind2=" ">
            <subfield code="f">629846@celes.unizar.es</subfield>
        </datafield>
        <datafield tag="856" ind1="4" ind2=" ">
            <subfield code="s">3329125</subfield>
            <subfield code="u">http://zaguan.unizar.es/record/58756/files/TAZ-TFM-2016-230.pdf</subfield>
            <subfield code="y">Memoria (spa)</subfield>
        </datafield>
        <datafield tag="909" ind1="C" ind2="O">
            <subfield code="o">oai:zaguan.unizar.es:58756</subfield>
            <subfield code="p">driver</subfield>
            <subfield code="p">trabajos-fin-master</subfield>
        </datafield>
        <datafield tag="950" ind1=" " ind2=" ">
            <subfield code="a"></subfield>
        </datafield>
        <datafield tag="951" ind1=" " ind2=" ">
            <subfield code="a">deposita:2017-01-26</subfield>
        </datafield>
        <datafield tag="980" ind1=" " ind2=" ">
            <subfield code="a">TAZ</subfield>
            <subfield code="b">TFM</subfield>
            <subfield code="c">CIEN</subfield>
        </datafield>
    </record>

    
</collection>