{"id":4072,"date":"2024-01-07T14:45:21","date_gmt":"2024-01-07T14:45:21","guid":{"rendered":"https:\/\/craterre.org\/?p=4072"},"modified":"2024-09-26T08:08:04","modified_gmt":"2024-09-26T08:08:04","slug":"soutenance-de-these-de-andy-combey-15-mars-en-ligne","status":"publish","type":"post","link":"https:\/\/craterre.org\/en\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/","title":{"rendered":"Soutenance de th\u00e8se de Andy Combey (15 mars, en ligne)"},"content":{"rendered":"

Vous \u00eates chaleureusement convi\u00e9s \u00e0 la\u00a0soutenance de th\u00e8se d\u2019Andy Combey<\/strong>, doctorant du laboratoire\u00a0ISTerre\u00a0<\/a>\/ UGA co-encadr\u00e9 par l\u2019Unit\u00e9 de recherche AE&CC, qui se d\u00e9roulera le\u00a0mardi 15 Mars \u00e0 14h<\/strong>\u00a0dans l\u2019amphith\u00e9\u00e2tre de l\u2019INRAE<\/strong>\u00a0(2 Rue de la Papeterie, 38402 Saint-Martin-d\u2019H\u00e8res).<\/p>\n

La soutenance sera \u00e9galement diffus\u00e9e en direct via le lien ci-dessous :
\nhttps:\/\/univ-grenoble-alpes-fr.zoom.us\/j\/98056625753?pwd=cGhvdm5zc2RpOVJnWEMwbDdWVVBHUT09<\/a>
\nID de r\u00e9union\u00a0: 980 5662 5753
\nCode secret\u00a0: 830342<\/p>\n

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Directeur et co-directeur<\/strong><\/h4>\n

Mrs.\u00a0Laurence AUDIN<\/strong>, Directrice de recherche, IRD (Directrice de th\u00e8se)
\nMr.\u00a0David GANDREAU<\/strong>, Docteur en sciences, ENSAG (Co-encadrant de th\u00e8se)<\/p>\n

 <\/p>\n

Membres du jury<\/strong><\/h4>\n

M.\u00a0Chris GERRARD<\/strong>, Professeur, Durham University (Rapporteur)
\nMr.\u00a0Gerardo SU\u00c1REZ<\/strong>, Directeur de recherche, Universidad Nacional Aut\u00f3noma de M\u00e9xico (Rapporteur)
\nMr.\u00a0Daniel H. SANDWEISS<\/strong>, Professeur, University of Maine (Examinateur)
\nMr.\u00a0Rohit JIGYASU<\/strong>, Chef de projet, ICCROM (Examinateur)
\nMr.\u00a0Thierry CAMELBEECK<\/strong>, Docteur en sciences, Observatoire Royal de Belgique (Examinateur) Mrs.\u00a0Julia DE SIGOYER<\/strong>, Professeure des universit\u00e9s, UGA (Examinatrice \u2013 Pr\u00e9sidente)<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

 <\/p>\n<\/section>\n

 <\/p>\n

\n
\n

Approche arch\u00e9osismologique dans le berceau des Incas (Cusco, P\u00e9rou). Potentialit\u00e9s et limites pour l\u2019\u00e9valuation de l\u2019al\u00e9a sismique actuel et la perception pass\u00e9e du risque tellurique<\/h3>\n<\/div>\n

Face \u00e0 l\u2019exposition croissante de nos soci\u00e9t\u00e9s aux tremblements de terre, une \u00e9valuation pr\u00e9cise de l\u2019al\u00e9a sismique s\u2019av\u00e8re \u00eatre une imp\u00e9rieuse n\u00e9cessit\u00e9. Identifier les marqueurs de la sismicit\u00e9 dans le registre arch\u00e9ologique est d\u00e9sormais reconnu comme une approche pertinente afin de combler le foss\u00e9 entre la pal\u00e9osismologie et la sismicit\u00e9 historique\/instrumentale. Pourtant, cette discipline demeure cantonn\u00e9e au bassin m\u00e9diterran\u00e9en.<\/p>\n

A la diff\u00e9rence de la frange Pacifique soumise aux fr\u00e9quents et bien circonscrits s\u00e9ismes de subduction, la r\u00e9gion de Cusco au P\u00e9rou est principalement affect\u00e9e par une sismicit\u00e9 crustale mod\u00e9r\u00e9e mais diffuse. Cette derni\u00e8re repr\u00e9sente un danger latent et un al\u00e9a tr\u00e8s largement sous-estim\u00e9. La r\u00e9gion est \u00e9galement le berceau de la culture inca et de son architecture en pierre monumentale, pr\u00e9tendument parasismique. Ce patrimoine offre donc une opportunit\u00e9 unique d\u2019\u00e9largir le catalogue sismique, mieux comprendre la dynamique des failles r\u00e9gionales et am\u00e9liorer notre compr\u00e9hension de la perception\/gestion des tremblements de terre \u00e0 l\u2019\u00e9poque inca. Dans le cadre de ce travail de th\u00e8se original nous pr\u00e9sentons les r\u00e9sultats de la premi\u00e8re \u00e9tude arch\u00e9osismologique de grande ampleur en Am\u00e9rique du Sud. Cette d\u00e9marche
\ntransdisciplinaire inclue une prospection sur 17 sites incas, la conception\/r\u00e9alisation d\u2019un syst\u00e8me de collecte et de gestion des donn\u00e9es de terrain et la r\u00e9interpr\u00e9tation d\u2019un r\u00e9cit l\u00e9gendaire de la tradition orale pr\u00e9colombienne. En outre, nous avons \u00e9labor\u00e9 une m\u00e9thodologie permettant l\u2019analyse vibratoire de structures massives en pierre, sur un cas d\u2019\u00e9tude en France lors de la crise sismique du Teil (2019) et avant son application \u00e0 Cusco.<\/p>\n

Avec plus de 3000 dommages sismiques identifi\u00e9s, les r\u00e9sultats obtenus d\u00e9montrent, en premier lieu, la capacit\u00e9 des \u00e9difices incas \u00e0 enregistrer des s\u00e9ismes. Les donn\u00e9es historiques sugg\u00e8rent d\u2019ailleurs un seuil de sensibilit\u00e9 proche de VIII en terme d\u2019intensit\u00e9 sismique de ce type de construction. La grande majorit\u00e9 des d\u00e9formations enregistr\u00e9es dans le b\u00e2ti en \u00e9l\u00e9vation t\u00e9moigne donc de l\u2019occurrence d\u2019un, ou plusieurs, s\u00e9ismes plus violents que ceux recens\u00e9s depuis 1650. L\u2019interpr\u00e9tation combin\u00e9e des donn\u00e9es de terrain et des donn\u00e9es ethnohistoriques supporte l\u2019existence, d\u2019au moins un s\u00e9isme majeur (Mw6.5) durant la phase imp\u00e9riale inca (1400-1533 CE), associ\u00e9 \u00e0 la rupture en surface du segment de faille Tambomachay-Pachatusan bordant le nord du bassin de Cusco. Enfin, notre travail souligne l\u2019int\u00e9r\u00eat des m\u00e9thodes de vibrations ambiantes pour caract\u00e9riser le comportement dynamique des structures arch\u00e9ologiques et interroger la conception parasismique de l\u2019architecture inca.<\/p>\n

Compte tenu des r\u00e9sultats obtenus, ce manuscrit pose les bases d\u2019une analyse renouvel\u00e9e des interactions entre populations pr\u00e9colombiennes et sismicit\u00e9, et plaide pour un d\u00e9veloppement accru de l\u2019arch\u00e9osismologie et de la pal\u00e9osismologie dans les Hautes Terres andines, et \u00e0 plus grande \u00e9chelle en Am\u00e9rique du Sud o\u00f9 cette approche n\u2019a pas encore \u00e9t\u00e9 mise en \u0153uvre.<\/p>\n<\/div>","protected":false},"excerpt":{"rendered":"

Vous \u00eates chaleureusement convi\u00e9s \u00e0 la\u00a0soutenance de th\u00e8se d\u2019Andy Combey, […]<\/p>","protected":false},"author":1,"featured_media":4071,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"yoast_head":"\nSoutenance de th\u00e8se de Andy Combey (15 mars, en ligne) - CRAterre<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/craterre.org\/en\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Soutenance de th\u00e8se de Andy Combey (15 mars, en ligne) - CRAterre\" \/>\n<meta property=\"og:description\" content=\"Vous \u00eates chaleureusement convi\u00e9s \u00e0 la\u00a0soutenance de th\u00e8se d\u2019Andy Combey, […]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/craterre.org\/en\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/\" \/>\n<meta property=\"og:site_name\" content=\"CRAterre\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/centrecraterre\" \/>\n<meta property=\"article:published_time\" content=\"2024-01-07T14:45:21+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2024-09-26T08:08:04+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/craterre.org\/wp-content\/uploads\/2024\/01\/Soutenance-de-these-de-Andy-Combey-15-mars-en-ligne.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"400\" \/>\n\t<meta property=\"og:image:height\" content=\"225\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"author\" content=\"admin\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"admin\" \/>\n\t<meta name=\"twitter:label2\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"4 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\/\/craterre.org\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/#article\",\"isPartOf\":{\"@id\":\"https:\/\/craterre.org\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/\"},\"author\":{\"name\":\"admin\",\"@id\":\"https:\/\/craterre.org\/#\/schema\/person\/6e8db622dd58bc34c3ae0154cf76e099\"},\"headline\":\"Soutenance de th\u00e8se de Andy Combey (15 mars, en ligne)\",\"datePublished\":\"2024-01-07T14:45:21+00:00\",\"dateModified\":\"2024-09-26T08:08:04+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\/\/craterre.org\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/\"},\"wordCount\":745,\"commentCount\":0,\"publisher\":{\"@id\":\"https:\/\/craterre.org\/#organization\"},\"articleSection\":[\"Archives\"],\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"CommentAction\",\"name\":\"Comment\",\"target\":[\"https:\/\/craterre.org\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/#respond\"]}]},{\"@type\":\"WebPage\",\"@id\":\"https:\/\/craterre.org\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/\",\"url\":\"https:\/\/craterre.org\/archives\/soutenance-de-these-de-andy-combey-15-mars-en-ligne\/\",\"name\":\"Soutenance de th\u00e8se de Andy Combey (15 mars, en ligne) - 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