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To achieve this, tsunami deposit thicknesses from over 150 cores collected at Salgados in southern Portugal were compared to the results of a tsunami sediment transport model (Delft3D\u2010FLOW) that simulates tsunami propagation, inundation, erosion, and deposition. Five different hypothetical seismic sources were modeled with varying bed roughness coefficients to assess how well they reproduced observed patterns of tsunami deposit thicknesses and dune. Modeled and observed historical tsunami arrival times were also used to test different earthquake sources. Based on these comparisons, three modeled earthquake sources were able to reproduce the observed data, suggesting they should be regarded as somewhat more likely sources for the 1755 earthquake in contrast to four other modeled sources. The fault closest to shore (Marqu\u00eas de Pombal) yielded the best correlations between model and observations.<\/jats:p>","DOI":"10.1029\/2020ea001109","type":"journal-article","created":{"date-parts":[[2021,2,6]],"date-time":"2021-02-06T11:39:06Z","timestamp":1612611546000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":8,"title":["Can Modeling the Geologic Record Contribute to Constraining the Tectonic Source of the 1755 CE Great Lisbon Earthquake?"],"prefix":"10.1029","volume":"8","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-0872-9715","authenticated-orcid":false,"given":"F.","family":"Dourado","sequence":"first","affiliation":[{"name":"CEPEDES Universidade do Estado do Rio de Janeiro  Rio de Janeiro Brazil"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6573-0539","authenticated-orcid":false,"given":"P. J. M.","family":"Costa","sequence":"additional","affiliation":[{"name":"Instituto Dom Luiz Faculdade de Ci\u00eancias Universidade de Lisboa  Lisboa Portugal"},{"name":"Departamento de Ci\u00eancias da Terra Faculdade de Ci\u00eancias e Tecnologia Universidade de Coimbra  Coimbra Portugal"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-4500-7885","authenticated-orcid":false,"given":"S.","family":"La Selle","sequence":"additional","affiliation":[{"name":"Pacific Coastal and Marine Science Center United States Geological Survey  Santa Cruz CA USA"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-8451-9437","authenticated-orcid":false,"given":"C.","family":"Andrade","sequence":"additional","affiliation":[{"name":"Departamento de Geologia Instituto Dom Luiz Faculdade de Ci\u00eancias Universidade de Lisboa  Portugal"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-7526-1841","authenticated-orcid":false,"given":"A. N.","family":"Silva","sequence":"additional","affiliation":[{"name":"Instituto Dom Luiz Faculdade de Ci\u00eancias Universidade de Lisboa  Lisboa Portugal"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-3977-6116","authenticated-orcid":false,"given":"I.","family":"Bosnic","sequence":"additional","affiliation":[{"name":"Instituto Dom Luiz Faculdade de Ci\u00eancias Universidade de Lisboa  Lisboa Portugal"}]},{"given":"G.","family":"Gelfenbaum","sequence":"additional","affiliation":[{"name":"Pacific Coastal and Marine Science Center United States Geological Survey  Santa Cruz CA USA"}]}],"member":"13","published-online":{"date-parts":[[2021,4,20]]},"reference":[{"key":"e_1_2_8_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.earscirev.2010.11.001"},{"key":"e_1_2_8_3_1","volume-title":"Inqu\u00e9rito do Marquez de Pombal (Ma\u00e7o No. 638)","author":"Arquivos do Minist\u00e9rio do Reino","year":"1756"},{"key":"e_1_2_8_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0264-3707(97)00019-7"},{"key":"e_1_2_8_5_1","doi-asserted-by":"publisher","DOI":"10.5194\/nhess-3-333-2003"},{"key":"e_1_2_8_6_1","doi-asserted-by":"publisher","DOI":"10.5194\/nhess-11-3319-2011"},{"key":"e_1_2_8_7_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0079-1946(97)00011-6"},{"issue":"1","key":"e_1_2_8_8_1","first-page":"9","article-title":"Maximum entropy analysis of Portuguese tsunami data: The tsunamis of 28.02.1969 and 26.05.1975","volume":"10","author":"Baptista M. 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