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    <titleInfo>
      <title>Groundwater in ultramatic mined massifs of New Caledonia</title>
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    <name type="personnal">
      <namePart type="family">Join</namePart>
      <namePart type="given">J.L.</namePart>
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    <name type="personnal">
      <namePart type="family">Ambrosi</namePart>
      <namePart type="given">Jean-Paul</namePart>
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    <abstract>Groundwater in ultramatic mined massifs of New Caledonia. Ultramafic rocks outcrop over more than one third of New Caledonia's main island. Under tropical conditions, thick lateritic mantles with nickel concentrations developed on these rocks by geochemical weathering. Groundwater in ultramafic mined massifs represents a valuable resource, but also a severe constrain for mining engineering. Previous works describe several water tables in the various layers of the weathering mantle. From a hydrologic study of the Tiebaghi massif, the hydraulic continuity across the weathering layers down to the bedrock is proposed.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>aquifer</topic>
      <topic>ultramafic rock</topic>
      <topic>mine</topic>
      <topic>regolith</topic>
      <topic>New Caledonia</topic>
    </subject>
    <classification authority="local">068</classification>
    <classification authority="local">062</classification>
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      <titleInfo>
        <title>Comptes Rendus Geoscience</title>
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      <part>
        <detail type="volume">
          <number>337</number>
        </detail>
        <detail type="volume">
          <number>16</number>
        </detail>
        <extent unit="pages">
          <list> 1500-1508</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2005</dateIssued>
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      <identifier type="issn">1631-0713</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010035842</identifier>
    <identifier type="doi">10.1016/j.crte.2005.08.011</identifier>
    <identifier type="issn">1631-0713</identifier>
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