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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Metamorphic Rocks</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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              <elementText elementTextId="3237">
                <text>This collection includes slates, phyllites, schists, gneisses, eclogites, marbles, quartzites, skarns, granulites, and mylonites.</text>
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            <name>Creator</name>
            <description>An entity primarily responsible for making the resource</description>
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                <text>Bereket Haileab</text>
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          <element elementId="48">
            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
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                <text>Housed in Anderson Hall, Carleton College.</text>
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            <name>Format</name>
            <description>The file format, physical medium, or dimensions of the resource</description>
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                <text>Thin sections, thin section scans, hand samples, hand sample images, photomicrographs, chemical analyses (major elements, trace elements and REE analyses for selected samples).</text>
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    <name>Thin section and hand sample</name>
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          <name>Title</name>
          <description>A name given to the resource</description>
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              <text>BH250-48</text>
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          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Gneiss</text>
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          <name>Description</name>
          <description>An account of the resource</description>
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              <text>Major Mineral: Allanite&#13;
Other Major Minerals: Microcline, orthoclase, biotite, quartz, perthite&#13;
&#13;
Mineralogical Comments:&#13;
Very large allanite crystals are present and show significant alteration. Myrmekite is common in association with feldspars.&#13;
&#13;
Alteration:&#13;
Allanite is extensively altered, displaying patchy zoning, partial replacement rims, and loss of interference colors. Signs of metamictization and radiation damage are evident, including pleochroic halos around radioactive inclusions.</text>
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          <name>Coverage</name>
          <description>The spatial or temporal topic of the resource, the spatial applicability of the resource, or the jurisdiction under which the resource is relevant</description>
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              <text>Location: Beartooth Mountains, Wyoming, USA&#13;
GPS Coordinates:  44°55'38.67"N, 109°43'37.45"W&#13;
Nearby Geography: Beartooth Mountains&#13;
Collected during petrology field trip in 2000</text>
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          <name>Source</name>
          <description>A related resource from which the described resource is derived</description>
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              <text>From the rock collection of Bereket Haileab. Sample BH250-48. Housed at Carleton College in Minnesota.</text>
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          <name>Type</name>
          <description>The nature or genre of the resource</description>
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              <text>Thin section and hand sample</text>
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          <description>A related resource</description>
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              <text>Bereket Haileab</text>
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          <name>Contributor</name>
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              <text>Bereket Haileab</text>
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      <name>allanite</name>
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      <name>allanite alteration</name>
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      <name>Beartooth Mountains</name>
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    <tag tagId="34">
      <name>gneiss</name>
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    <tag tagId="560">
      <name>high-grade metamorphism</name>
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      <name>loss of interference colors</name>
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      <name>metamictization</name>
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    <tag tagId="1">
      <name>metamorphic</name>
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      <name>microcline</name>
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      <name>myrmekite</name>
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    <tag tagId="565">
      <name>patchy zoning</name>
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    <tag tagId="563">
      <name>REE-bearing minerals</name>
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    <tag tagId="566">
      <name>replacement rims</name>
    </tag>
    <tag tagId="556">
      <name>Wyoming geology</name>
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