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        <identifier>oai:meral.edu.mm:recid/291</identifier>
        <datestamp>2021-12-13T00:39:24Z</datestamp>
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          <dc:title>Estimation of Sedimentary Layered Media at Prambanan Area, Yogyakarta Indonesia</dc:title>
          <dc:creator>Pyi Soe Thein</dc:creator>
          <dc:creator>Subagyo Pramumijoyo</dc:creator>
          <dc:description>In this study, we investigated the sedimentary layered media at Prambanan area, Yogyakarta.&#13; Several powerful earthquakes have struck the Opak River Fault during recent years. An&#13; earthquake occurred at Sengir village, Prambanan District, Yogyakarta on May 27, 2006, and&#13; caused several casualties. Following the event, we conducted a microtremor survey to&#13; estimate the shaking intensity distribution during the earthquake. We performed single&#13; observations of microtremor at 124 sites in Prambanan area. We also conducted 2-site bore&#13; holes investigation to gain a representative determination of the soil condition of subsurface&#13; structures in Prambanan. From the Standard Peneration Tests (SPT) of borehole observations,&#13; the prambanan area corresponds to relatively soil condition with Vs 298 m/s, the predominant&#13; periods due to horizontal vertical ratios (HVSRs) are in the range of 0.95 to 1.92 s and the&#13; frequency are in the range of 0.48 to 1.19 Hz. By making these observations, we can obtain a&#13; relationship between predominant periods, frequency, general soil types and peak ground&#13; acceleration. The results enabled us to estimate the site-dependent shaking characteristics of&#13; earthquake ground motion.</dc:description>
          <dc:date>2019</dc:date>
          <dc:identifier>http://hdl.handle.net/20.500.12678/0000000291</dc:identifier>
          <dc:identifier>https://meral.edu.mm/records/291</dc:identifier>
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