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  <titleInfo>
    <title>Analysis of the extent and the distribution of aquifers</title>
    <subTitle>in the Chao Phraya Basin, Thailand</subTitle>
  </titleInfo>
  <name type="personal">
    <namePart>Piyasena, Wije Munige</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Prinya Nutalaya</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Akagi, Toshinobu</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Campbell, K.V.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Government of Australia</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <genre authority="marc">series</genre>
  <genre authority="marc">technical report</genre>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1979</dateIssued>
    <issuance>continuing</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <extent>vi, 186 p.</extent>
  </physicalDescription>
  <abstract>A thorough analysis of lithologic logs of ground water wells in Bangkok area was carried out by using a systematic correlation procedure based on matching technique utilizing a series of computer programs in order to delineate the stratigray of Bangkok subsoils. Several east-west and north-south  stratigraphic cross sections were established and through a detailed analysis of these cross sections, three partially separated sand layers were identified within first 150 m depth. Trend surfaces were fitted to establish trends associated with top and bottom surfaces and were used to analyze thickness variation of each sand layer. Finally, a table giving a detailed description of sand layers was prepared.</abstract>
  <note>A thesis submitted in partial fulfilment of the requirements for the degree of Master of Engineering, School of Engineering and Technology</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1979</note>
  <subject authority="lcsh">
    <topic>Aquifers</topic>
    <topic>Thailand</topic>
    <topic>Bangkok</topic>
  </subject>
  <relatedItem type="series">
    <titleInfo>
      <title>Thesis ; no. GT-78-26</title>
    </titleInfo>
    <name type="corporate">
      <namePart>Asian Institute of Technology.</namePart>
      <namePart/>
    </name>
  </relatedItem>
  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B22269</identifier>
  <location>
    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B22269</url>
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  <recordInfo>
    <recordCreationDate encoding="marc">121096</recordCreationDate>
    <recordChangeDate encoding="iso8601">20260817162451.0</recordChangeDate>
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