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		<title>J. Perez-Cuevas 2021a - Revision history</title>
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		<title>Scipediacontent: Scipediacontent moved page Draft Content 323251079 to J. Perez-Cuevas 2021a</title>
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				<updated>2021-11-30T11:52:39Z</updated>
		
		<summary type="html">&lt;p&gt;Scipediacontent moved page &lt;a href=&quot;/public/Draft_Content_323251079&quot; class=&quot;mw-redirect&quot; title=&quot;Draft Content 323251079&quot;&gt;Draft Content 323251079&lt;/a&gt; to &lt;a href=&quot;/public/J._Perez-Cuevas_2021a&quot; title=&quot;J. Perez-Cuevas 2021a&quot;&gt;J. Perez-Cuevas 2021a&lt;/a&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 11:52, 30 November 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan='2' style='text-align: center;' lang='en'&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
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	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=J._Perez-Cuevas_2021a&amp;diff=232674&amp;oldid=prev</id>
		<title>Scipediacontent: Created page with &quot;== Abstract ==  Hispaniola is in the edge of interaction between the North American and Caribbean  plates. In this zone, the occurrence of earthquakes greater than 5.0, Mw is...&quot;</title>
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				<updated>2021-11-30T11:52:36Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot;== Abstract ==  Hispaniola is in the edge of interaction between the North American and Caribbean  plates. In this zone, the occurrence of earthquakes greater than 5.0, Mw is...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;== Abstract ==&lt;br /&gt;
&lt;br /&gt;
Hispaniola is in the edge of interaction between the North American and Caribbean &lt;br /&gt;
plates. In this zone, the occurrence of earthquakes greater than 5.0, Mw is frequent, &lt;br /&gt;
characterizing  it as  a seismically active  zone. These earthquakes cause considerable material &lt;br /&gt;
damage  and  can  provoke  loss  of  human  lives.  The  Cathedral  of  Santo  Domingo,  Primate  of &lt;br /&gt;
the  Americas,  is  in  the  Colonial  City  of  Santo  Domingo.  It  is  the  most  important  colonial &lt;br /&gt;
building  in  Dominican  Republic,  was  built  between  1521-1541,  and  is  a  masonry  building &lt;br /&gt;
made  with  stone  ashlars  and  covered  with  stone  ribbed  vault.  However,  it  is  essential  to &lt;br /&gt;
know  about  the  possible  seismic  behavior  that  the  ground  could  have  in  case  of  a  relevant &lt;br /&gt;
earthquake to try to avoid  possible  damage  to  this  heritage.  For  this  reason,  the  aim  of  this &lt;br /&gt;
research  is  to  apply geophysical prospecting methods for the seismic site characterization of &lt;br /&gt;
the Cathedral of Santo Domingo.  For  this  study,  the  geophysical  methods applied  were: &lt;br /&gt;
MASW  (Multichannel Analysis  of  Surface  Wave),  H/V  Spectral  Ratio  and  Georadar.  The &lt;br /&gt;
characterization  of  site conditions was determined with the values of the average shear wave &lt;br /&gt;
velocity for the top 30 m of  soil  (Vs30)  obtained  with  the  MASW  method.  As  a  main  result &lt;br /&gt;
it  was  found  that  the  site  seismic  class  determined  with  the  MASW  method  was  type  C-&lt;br /&gt;
very  dense  soil  and  soft  rock  (360-760  m/s),  according  to  the  NEHRP  classification.  In &lt;br /&gt;
addition,  the  Georadar  tests  allowed  confirming  that  there  are  no  unknown  caverns  in  the &lt;br /&gt;
basement of the Cathedral in the first 5 m, thus it is accepted as valid the seismic &lt;br /&gt;
classification of the soil obtained by the MASW method.&lt;br /&gt;
&lt;br /&gt;
== Full document ==&lt;br /&gt;
&amp;lt;pdf&amp;gt;Media:Draft_Content_323251079p722.pdf&amp;lt;/pdf&amp;gt;&lt;br /&gt;
== References ==&lt;br /&gt;
&lt;br /&gt;
[1]  Sabrina,  G.,  Sebastiano,  I.,  Graziano,  P.,  Domenico,  B.,  Giuseppe,  L.  and  Francesco,  P. Geophysical surveys for the dynamic characterization of a cultural heritage building and its subsoil: The S. Michele Arcangelo Church (Acireale, eastern Sicily). Journal of Cultural Heritage, 36 (2019) 72-84. https://doi.org/10.1016/j.culher.2018.09.015  &lt;br /&gt;
&lt;br /&gt;
[2]  Baradello, L., Carcione, J.M. and Gei, D. Fast monostatic GPR modeling. Geophysics. 69 (2004), pp.466–471. Doi: 10.1190/1.1707066.  &lt;br /&gt;
&lt;br /&gt;
[3]  Barilaro,  D.,  Branca,  C.,  Gresta,  S.,  Imposa,  S.,  Leone,  A.  and  Majolino,  D.  Ground penetrating  radar  (G.P.R.)  surveys  applied  to  the  research  of  crypts in San Sebastiano’s church in Catania (Sicily). Journal of Cultural Heritage. 8, 73-76.  doi:10.1016/j.culher.2006.10.003  &lt;br /&gt;
&lt;br /&gt;
[4]  Castellaro, S., Imposa, S., Barone, F., Chiavetta. F., Gresta. S. and Mulargia, F. Georada  and  passive  seismic  survey  in  the  Roman  Amphitheatre  of  Catania  (Sicily).  Journal  of  Cultural Heritage, 9 (2008) 357-366. doi:10.1016/j.culher.2008.03.004 &lt;br /&gt;
&lt;br /&gt;
[5]  Leucci, G., De Giorgi, L., Di Giacomo, G., Ditaranto, I., Miccoli, I. and Scardozzi, G. 3D  GPR survey for the archaeological characterization of the ancient Messapian necropolis in  Lecce, South Italy, Journal of Archaeological Science: Reports, Reports 7 (2016) 290-302.  http://dx.doi.org/10.1016/j.jasrep.2016.05.027  &lt;br /&gt;
&lt;br /&gt;
[6]  Casas,  A.,  Cosentino,  P.  L.,  Fiandaca,  G.,  Himi,  M.,  Macias  Solé,  J.M.,  Martorana,  R., Muñoz, A., Rivero Rivero, L., Sala, R. and Teixell, I. Non-invasive Geophysical Surveys in Search of the Roman Temple of Augustus Under the Cathedral of Tarragona (Catalonia, Spain):  A  Case  Study,  Surveys  in  Geophysics,  April  2018.  doi.org/10.1007/s10712-018-9470-6  &lt;br /&gt;
&lt;br /&gt;
[7]  Di Giacomo, G., De Giorgi, L., Ditaranto, I., Leucci, G., Miccoli, I. and Scardozzi, G. The  Medieval cave village of Casalrotto (Mottola, Apulia): New data on the settlement and its  necropolis from archaeological and geophysical measurements, Measurement, 128 (2018)  96-103. https://doi.org/10.1016/j.measurement.2018.06.038   &lt;br /&gt;
&lt;br /&gt;
[8]  Park,  C.B.,  Miller,  R.D.,  Xia,  J.  and  Ivanov,  J.  Multichannel  analysis  of  surface  waves (MASW) active and passive methods”, in Kansas  Geological  Survey,  Lawrence,  USA, January 2007.  &lt;br /&gt;
&lt;br /&gt;
[9]  Anukwu, G.C., Khalil, A.E., Nawawi, M., Abdullah, K. and Abdullah, F.M. Multi-channel  analysis of surface waves (MASW) using CMP analysis to identify soil problems threat on  the heritage site at Georgetown, Malaysia, International Geophysical Conference, Beijing,  China, 24-27 April 2018. doi.org/10.1190/IGC2018-404   &lt;br /&gt;
&lt;br /&gt;
[10] Tarque,  N.,  Lai,  C.G.,  Bozzoni,  F.,  Miccadei,  E.,  Piacentini,  T.,  Camata,  G.  and  Spacone, E. Expected ground motion at the historical site of Poggio Picenze, Central Italy,  with reference to current Italian building code, Engineering Geology, 166 (2013) 100-115.  http://dx.doi.org/10.1016/j.enggeo.2013.09.003.  &lt;br /&gt;
&lt;br /&gt;
[11] Cercato,  M.,  De  Donno,  G.,  di  Giulio,  A.,  Lanzo,  G.  y  Tommasi,  P.  Dynamic  Characterization  of  the  hill  of  Civita  di  Bagnoregio  (Viterbo,  Central  Italy)  for  seismic  response analysis. Engineering Geology (2019),  https://doi.org/10.1016/j.enggeo.2019.105463  &lt;br /&gt;
&lt;br /&gt;
[12] Flores  Sasso,  V.  and  Prieto  Vicioso,  E.  El  modelo  Hallemkirche  o  iglesia  salón  en  el reino de Castilla de Ultramar. La Catedral de Santo Domingo, in &amp;quot;Obra Congrua, 1416. 500 aniversario de la Consulta de la Catedral de Girona, Universidad de Girona, Departamento  de  Arquitectura  e  Ingeniería  de  la  Construcción,  Colegio  de  Aparejadores,  Arquitectos  Técnicos e Ingenieros de la Edificación de Girona. 2017. pp. 183-1992.   &lt;br /&gt;
&lt;br /&gt;
[13] Park, C. B., Miller, R. D., and Xia, J. (1999). Multichannel analysis of surface waves.  Geophysics, 64, 800–808.  &lt;br /&gt;
&lt;br /&gt;
[14] Xia, J., Park, C. B., Hunter, J. A., Harris, J. B., and Ivanov, J. (2002). Comparing shear- velocity profiles from multichannel analysis of surface wave with borehole  measurement. Soild Dynamics and Earthquake Engineering (SDEE), 22(3), 181–190.  &lt;br /&gt;
&lt;br /&gt;
[15] Nakamura,  Y.  (1989).  A  method  for  dynamic  characteristics  estimation  of  subsurface using  microtremors  on  the  ground  surface.  Quarterly  Report  of  Railway  Technical Research Institute (RTRI): 3, 25-33.  &lt;br /&gt;
&lt;br /&gt;
[16] Byeong-Jin P., Jeongguk K., Jaesun L., Man-Sung K. and Yun-Kyu A. Underground  Object Classification for Urban Roads Using Instantaneous Phase Analysis of Ground- Penetrating Radar (GPR) Data. Remote Sensing 10(9): 1417 (2018)  &lt;br /&gt;
&lt;br /&gt;
[17] Konno,  K.,  and  Ohmachi,  T.  (1998).  &amp;quot;Ground-motion  characteristic  estimated  from  Spectral Radio between Horizontal and Vertical Components of Microtremors&amp;quot;. Bulletin  of the Seismological Society of America: 88, 228-241.&lt;/div&gt;</summary>
		<author><name>Scipediacontent</name></author>	</entry>

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