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      <src>https://theses.otagogeology.org.nz/files/original/4e8000b625ebc0ab42d27b15ae85495d.pdf</src>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Geology theses</text>
              </elementText>
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    <name>OU Geology thesis</name>
    <description>Thesis or dissertation completed by University of Otago Geology students</description>
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      <element elementId="52">
        <name>Author last name</name>
        <description>Last name of the Author</description>
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          <elementText elementTextId="30524">
            <text>Morris</text>
          </elementText>
        </elementTextContainer>
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      <element elementId="53">
        <name>Project type</name>
        <description>Is it an MSc, PhD, BSc(Hons) or PGDipSci?</description>
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          <elementText elementTextId="30527">
            <text>BSc(Hons)</text>
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      <element elementId="54">
        <name>Advisers</name>
        <description>Who supervised/advised this student</description>
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          <elementText elementTextId="30529">
            <text>Duggan, M.B.</text>
          </elementText>
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      <element elementId="55">
        <name>Abstract</name>
        <description>The Abstract for this thesis</description>
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          <elementText elementTextId="30530">
            <text>Campbell Island owes its origin largely to Upper Miocene volcanism. Volcanic flow rocks cover approximately two thirds of the island, having been derived from a volcanic centre to the west of the island, which has been removed by marine erosion. Onland flows have been modified by radial drainage channels developed about the volcanic centre. 
The flow rocks are dominantly hawaiitic to mugearitic,with a smaller number of more evolved flows of the alkali olivine basalt lineage. Intrusive rocks are mineralogically and chemically similar to the flow rocks. Both are characterised by mineralogical and chemical homogeneity, but textural variety. 
The igneous rocks are believed to have been derived from melting of the mantle to produce an alkali basaltic parent,which has undergone subsequent fractional crystallisation,producing the observed rocks. 
There is little post eruptional structural modification, apart from the tilting of the Filhol Peak block.</text>
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      <element elementId="59">
        <name>Department</name>
        <description>The department where the student is studying primarily.</description>
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            <text>Geology</text>
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      <element elementId="61">
        <name>Named locality</name>
        <description>Named locality describing the field area location.</description>
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            <text>Campbell Island</text>
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      <element elementId="60">
        <name>Thesis description</name>
        <description>Number of pages, maps, CDs, etc.</description>
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          <elementText elementTextId="30536">
            <text>74 leaves : illus., 2 maps in pocket ; 30 cm.</text>
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      <name>Dublin Core</name>
      <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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        <element elementId="43">
          <name>Identifier</name>
          <description>An unambiguous reference to the resource within a given context</description>
          <elementTextContainer>
            <elementText elementTextId="30523">
              <text>1976Morris</text>
            </elementText>
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        <element elementId="39">
          <name>Creator</name>
          <description>An entity primarily responsible for making the resource</description>
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            <elementText elementTextId="30525">
              <text>Morris, Paul (Paul Andrew)</text>
            </elementText>
          </elementTextContainer>
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        <element elementId="40">
          <name>Date</name>
          <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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            <elementText elementTextId="30526">
              <text>1976</text>
            </elementText>
          </elementTextContainer>
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        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
          <elementTextContainer>
            <elementText elementTextId="30528">
              <text>Igneous geology of Campbell Island, Southwest Pacific Ocean.</text>
            </elementText>
          </elementTextContainer>
        </element>
        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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            <elementText elementTextId="30533">
              <text>Map</text>
            </elementText>
            <elementText elementTextId="30534">
              <text> Igneous petrology</text>
            </elementText>
            <elementText elementTextId="30535">
              <text> Mineralogy</text>
            </elementText>
          </elementTextContainer>
        </element>
      </elementContainer>
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    <tag tagId="138">
      <name>dyke</name>
    </tag>
    <tag tagId="229">
      <name>hawaiite-mugerite flows</name>
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