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  <responseDate>2026-05-31T12:37:05Z</responseDate>
  <request verb="GetRecord" identifier="oai:meral.edu.mm:recid/00008405" metadataPrefix="oai_dc">https://meral.edu.mm/oai</request>
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      <header>
        <identifier>oai:meral.edu.mm:recid/00008405</identifier>
        <datestamp>2022-11-29T08:44:28Z</datestamp>
        <setSpec>1582963788001:1582966668038</setSpec>
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      <metadata>
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          <dc:title>"Tectonic Implication of Letpangon-Thandaung Area, Pyin-Oo-Lwin Township, Mandalay Region"</dc:title>
          <dc:creator>Marlar Aye Shwe</dc:creator>
          <dc:creator>Maung Maung</dc:creator>
          <dc:creator>Maung Maung</dc:creator>
          <dc:description>"The study area is situated about 15 miles south of Pyin Oo Lwin Township, Mandalay
Region. It lies between latitude 21° 43´N to 21° 51´ N and longitude 96° 20´E to 96° 26´ E
of one-inch topographic maps 93- C/5 and 93 C/6. The present area is situated about 17
km long in N-S direction, 11 km wide in E-W direction. The Paleozoic strata from Late
Precambrian to Middle Devonian - Permian units are exposed in this area. This study is
mainly emphasized on the tectonic implication of the area. The tectonic setting of
Myanmar Region is related to the subduction of the northeast moving Indian Plate
beneath the Sibumsu that initially activated at the Mesozoic. In the area, the feature of
strike is a regional overthrust with a sinous outline, running N-S. The type of folds are
Myebon and Pondaung anticlines of younging downward antiforms and Son-baw-aing
syncline of younging upward synform. Several brittle and ductile deformations have
been recognized both on an outcrop and regional scale."</dc:description>
          <dc:date>2022-08-12</dc:date>
          <dc:identifier>https://meral.edu.mm/records/8405</dc:identifier>
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