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  <titleInfo>
    <title>Sedimentology of the Upper Cretaceous rocks of Todilto Park, New Mexico</title>
  </titleInfo>
  <name type="personal">
    <namePart>Willard, Max Emery</namePart>
    <namePart type="date">1914-</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <genre authority="marc">bibliography</genre>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">nmu</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Socorro</placeTerm>
    </place>
    <publisher>State Bureau of Mines and Mineral Resources, New Mexico Institute of Mining and Technology</publisher>
    <dateIssued>1964</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <form authority="marcform">print</form>
    <extent>44, [3] p. illus., col. maps, diagrs., tables 29 cm.</extent>
  </physicalDescription>
  <note type="statement of responsibility">By Max E. Willard.</note>
  <note>Bibliography:  p. [46]</note>
  <subject authority="lcsh">
    <topic>Sediments (Geology)</topic>
    <geographic>New Mexico</geographic>
    <geographic>Todilto Park</geographic>
  </subject>
  <subject authority="lcsh">
    <topic>Geology, Stratigraphic</topic>
    <temporal>Cretaceous</temporal>
  </subject>
  <subject authority="lcsh">
    <topic>Geology</topic>
    <geographic>New Mexico</geographic>
    <geographic>Todilto Park</geographic>
  </subject>
  <classification authority="lcc">QE471 .W52</classification>
  <identifier type="lccn">gs 64000216</identifier>
  <recordInfo>
    <recordContentSource authority="marcorg">U. S. Geol. Survey Libr.</recordContentSource>
    <recordCreationDate encoding="marc">760831</recordCreationDate>
    <recordChangeDate encoding="iso8601">20260227111414.0</recordChangeDate>
    <recordIdentifier source="DLC">gs 64000216 </recordIdentifier>
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