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  <titleInfo>
    <title>Geographinc Information System (GIS) aided design of Global Positioning System (GPS) network for monitoring crustal deformation in Mongolia</title>
  </titleInfo>
  <name type="personal">
    <namePart>Dambadarja, Enkhbaatar</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Honda, Kiyoshi</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Kaew Nualchawee</namePart>
    <role>
      <roleTerm type="text">Examination committee           </roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Delsol, Jean-Pierre</namePart>
    <role>
      <roleTerm type="text">Examination committee           </roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>French Government</namePart>
    <role>
      <roleTerm type="text">Scholarship donor</roleTerm>
    </role>
  </name>
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  <originInfo>
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    <place>
      <placeTerm type="text">Bangkok</placeTerm>
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    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1997</dateIssued>
    <issuance>monographic</issuance>
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  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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  <abstract>Mongolia marks the transition between predominantly north-south shortening in  the ~outh from collision of the Indian and Eurasian plates, east-western extension  asso~iated with the Baikal Rift system to the north. In this century western Mongolia has  been one of the most seismicaly active intracontinental regions in the world with four  earthquakes with magnitude (M) ~ 8 have occurred.  The dominant type of active faulting in western Mongolia is strike-slip in nature:  left-lateral on easterly trending planes in the 1905 Bulnay and Tsetserleg earthquakes and  the 1957 Gobi Altay and right-lateral on a north-north-westerly trending Fu-yun fault in  1931.  Geodetic measurements of the rates and styles of deformation throughout the  region would provide necessary constraints on models of central Asia, and will allow for  better understanding of earthquake processes in general and the future earthquake hazard  in Mongolia.  Active tectonic is to research intracontinental mountain building and territory of  Mongolia could be ideal field laboratory to conduct this type of investigation. For this  purpose it is suitable to research origin of fault, development, relationship of different fault  kinematics, exploration of formation. Most effective method with wide coverage in this  research can be occurred by GPS measurements. In order to conduct GPS estimation, it is  needed to s.et up several stations covering various areas of earthquake activity to conduct  measurements.</abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of  Master of  Science, School of Environment, Resources and Development </note>
  <note>Thesis (M.Sc.) - Asian Institute of Technology, 1997</note>
  <subject authority="lcsh">
    <topic>Geographic information systems</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Geodesy</topic>
    <geographic>Mongolia</geographic>
  </subject>
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    <titleInfo>
      <title>Thesis  no. SR-97-04</title>
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      <namePart>Asian Institute of Technology.</namePart>
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