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cdx-button--weight-quiet menu__item--page-actions-watch"> <span class="minerva-icon minerva-icon--star"></span> <span>Suivre</span> </a></li> <li id="page-actions-edit" class="page-actions-menu__list-item"><a role="button" id="ca-edit" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" data-event-name="menu.edit" data-mw="interface" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet edit-page menu__item--page-actions-edit"> <span class="minerva-icon minerva-icon--edit"></span> <span>Modifier</span> </a></li> </ul> </nav> <div id="mw-content-subtitle"></div> </div> <div id="bodyContent" class="content"> <div id="mw-content-text" class="mw-body-content"> <script>function mfTempOpenSection(id){var block=document.getElementById("mf-section-"+id);block.className+=" open-block";block.previousSibling.className+=" open-block";}</script> <div class="mw-content-ltr mw-parser-output" lang="fr" dir="ltr"> <section class="mf-section-0" id="mf-section-0"> <p>Le <b>rebond post-glaciaire</b> (également appelé <b>ajustement isostatique</b>, <b>rebond isostasique</b> ou <b>glacio-isostasie</b>) se définit comme le relèvement de masses terrestres consécutif à la déglaciation et plus précisément à la fonte des <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Calottes_glaciaires?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-redirect" title="Calottes glaciaires">calottes glaciaires</a>. Ces masses terrestres, antérieurement <i>déprimées</i> (par compression sous les charges de glace), se relèvent durant la période post-glaciaire du fait du phénomène d'<a href="https://fr-m-wikipedia-org.translate.goog/wiki/Isostasie?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Isostasie">isostasie</a>. Le terme de rebond a tendance à être remplacé par celui d'ajustement isostatique car il comprend, en plus du déplacement vertical, des mouvements horizontaux de la <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Lithosph%C3%A8re?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Lithosphère">lithosphère</a>, des variations du champ de gravité, et peut se traduire par des manifestations géologiques (réactivation du volcanisme, <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Sismicit%C3%A9?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-redirect" title="Sismicité">sismicité</a> induite).</p> <figure typeof="mw:File/Thumb"> <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Fichier:PGR_Paulson07_big.jpg?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/c/c9/PGR_Paulson07_big.jpg/300px-PGR_Paulson07_big.jpg" decoding="async" width="300" height="365" class="mw-file-element" srcset="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://upload.wikimedia.org/wikipedia/commons/thumb/c/c9/PGR_Paulson07_big.jpg/450px-PGR_Paulson07_big.jpg 1.5x,https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://upload.wikimedia.org/wikipedia/commons/thumb/c/c9/PGR_Paulson07_big.jpg/600px-PGR_Paulson07_big.jpg 2x" data-file-width="810" data-file-height="985"></a> <figcaption> Modélisation de l'ajustement post-glacial quaternaire : les zones en rouge se soulèvent en raison de la fonte des calottes glaciaires. Les zones bleues s'affaissent à cause du remplissage des bassins océaniques consécutif à cette fonte. </figcaption> </figure> <figure class="mw-default-size" typeof="mw:File/Thumb"> <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Fichier:Landhebung_in_Stockholm.jpg?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/5/5a/Landhebung_in_Stockholm.jpg/220px-Landhebung_in_Stockholm.jpg" decoding="async" width="220" height="182" class="mw-file-element" srcset="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://upload.wikimedia.org/wikipedia/commons/thumb/5/5a/Landhebung_in_Stockholm.jpg/330px-Landhebung_in_Stockholm.jpg 1.5x,https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://upload.wikimedia.org/wikipedia/commons/thumb/5/5a/Landhebung_in_Stockholm.jpg/440px-Landhebung_in_Stockholm.jpg 2x" data-file-width="3628" data-file-height="3000"></a> <figcaption> Les effets du rebond post-glaciaire à Stockholm. La carte indique l'accroissement des terres sur une période de 4000 ans. </figcaption> </figure> <p>À l'<a href="https://fr-m-wikipedia-org.translate.goog/wiki/%C3%89chelle_des_temps_g%C3%A9ologiques?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Échelle des temps géologiques">échelle des temps géologiques</a>, ce sont des mouvements très rapides (le rebond actuel est de l'ordre du centimètre par an<sup id="cite_ref-1" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-1"><span class="cite_crochet">[</span>1<span class="cite_crochet">]</span></a></sup>), qui peuvent avoir des impacts sismiques significatifs (réactivations de <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Faille?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Faille">failles</a><sup id="cite_ref-FailleReactivation2000_2-0" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-FailleReactivation2000-2"><span class="cite_crochet">[</span>2<span class="cite_crochet">]</span></a></sup>, <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Tremblements_de_terre?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-redirect" title="Tremblements de terre">tremblements de terre</a><sup id="cite_ref-DeglaciationImpacts2001_3-0" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-DeglaciationImpacts2001-3"><span class="cite_crochet">[</span>3<span class="cite_crochet">]</span></a></sup>).</p> <div id="toc" class="toc" role="navigation" aria-labelledby="mw-toc-heading"> <input type="checkbox" role="button" id="toctogglecheckbox" class="toctogglecheckbox" style="display:none"> <div class="toctitle" lang="fr" dir="ltr"> <h2 id="mw-toc-heading">Sommaire</h2><span class="toctogglespan"><label class="toctogglelabel" for="toctogglecheckbox"></label></span> </div> <ul> <li class="toclevel-1 tocsection-1"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#Dans_l'h%C3%A9misph%C3%A8re_nord"><span class="tocnumber">1</span> <span class="toctext">Dans l'hémisphère nord</span></a> <ul> <li class="toclevel-2 tocsection-2"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#Cons%C3%A9quences_sismiques"><span class="tocnumber">1.1</span> <span class="toctext">Conséquences sismiques</span></a></li> </ul></li> <li class="toclevel-1 tocsection-3"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#Indices_g%C3%A9ologiques"><span class="tocnumber">2</span> <span class="toctext">Indices géologiques</span></a></li> <li class="toclevel-1 tocsection-4"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#R%C3%A9f%C3%A9rences"><span class="tocnumber">3</span> <span class="toctext">Références</span></a></li> <li class="toclevel-1 tocsection-5"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#Voir_aussi"><span class="tocnumber">4</span> <span class="toctext">Voir aussi</span></a> <ul> <li class="toclevel-2 tocsection-6"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#Bibliographie"><span class="tocnumber">4.1</span> <span class="toctext">Bibliographie</span></a></li> <li class="toclevel-2 tocsection-7"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#Articles_connexes"><span class="tocnumber">4.2</span> <span class="toctext">Articles connexes</span></a></li> </ul></li> </ul> </div> </section> <div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(1)"> <span class="indicator mf-icon mf-icon-expand mf-icon--small"></span> <h2 id="Dans_l'hémisphère_nord"><span id="Dans_l.27h.C3.A9misph.C3.A8re_nord"></span>Dans l'hémisphère nord</h2><span class="mw-editsection"> <a role="button" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&section=1&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Modifier la section : Dans l'hémisphère nord" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>modifier</span> </a> </span> </div> <section class="mf-section-1 collapsible-block" id="mf-section-1"> <p>Cette partie du monde est la plus concernée, car dans l'hémisphère sud les zones continentales affectées par une déglaciation sont inexistantes, hormis la pointe de l'Amérique du sud. Autour du cercle polaire arctique, ce phénomène affecte plus directement les régions d'Europe septentrionale (en particulier l'<a href="https://fr-m-wikipedia-org.translate.goog/wiki/%C3%89cosse?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Écosse">Écosse</a>, la <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Fennoscandie?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Fennoscandie">Fennoscandie</a> et le nord du <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Danemark?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Danemark">Danemark</a>), la <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Sib%C3%A9rie?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Sibérie">Sibérie</a>, le <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Canada?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Canada">Canada</a> ainsi que les <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Grands_Lacs_(Am%C3%A9rique_du_Nord)?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Grands Lacs (Amérique du Nord)">Grands Lacs</a> du <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Canada?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Canada">Canada</a> et des <a href="https://fr-m-wikipedia-org.translate.goog/wiki/%C3%89tats-Unis?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="États-Unis">États-Unis</a>. Il affecte aussi les fonds marins, et en particulier celui de la <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Mer_du_Nord?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Mer du Nord">mer du Nord</a>.</p> <div class="mw-heading mw-heading3"> <h3 id="Conséquences_sismiques"><span id="Cons.C3.A9quences_sismiques"></span>Conséquences sismiques</h3><span class="mw-editsection"> <a role="button" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&section=2&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Modifier la section : Conséquences sismiques" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>modifier</span> </a> </span> </div> <ul> <li>À chaque déglaciation, le recul et l'allègement des calottes glaciaires en Amérique du Nord et en Europe septentrionale ont induit un <a href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=D%C3%A9s%C3%A9quilibre_isostatique&action=edit&redlink=1&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="new" title="Déséquilibre isostatique (page inexistante)">déséquilibre isostatique</a> dans les couches lithosphère–asthénosphère. Les régions libérées du poids de la glace se soulèvent et un « bombement isostatique » apparaît. Ce double phénomène est encore en cours après la fin de la <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Derni%C3%A8re_glaciation?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-redirect" title="Dernière glaciation">dernière glaciation</a>, accompagnant une modification des contraintes <i>intra-plaques</i> dans la zone de l'ancienne <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Calotte_glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Calotte glaciaire">calotte glaciaire</a>, et à sa périphérie, notamment dans le secteur norvégien de la mer du Nord septentrionale qui fait l'objet d'une prospection ou exploitation pétrolière et gazière. <br> La « flexure lithosphérique » est une cause probable <span class="citation">« de la séismicité anormalement élevée dans la zone sismique de New Madrid, près du Centre des États-Unis (où les taux de déformations actuels atteignent 10<sup>−9</sup>an<sup>−1</sup>, soit près de 1000 fois le taux de « déformation sismique » environnant, 10<sup>−12</sup> an<sup>−1</sup>)<sup id="cite_ref-DeglaciationImpacts2001_3-1" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-DeglaciationImpacts2001-3"><span class="cite_crochet">[</span>3<span class="cite_crochet">]</span></a></sup>. Cette zone a connu trois séismes extrêmement importants (M∼8) en 1811–1812, à la suite d'autres grands séismes survenus durant l'Holocène. Comme les sédiments tertiaires ne montrent pas de déformation significative dans ce secteur, la déglaciation constitue le facteur déclenchant le plus vraisemblable pour cette séismicité récente »</span> estimaient en 2001 Mark D. Zoback et Balz Grollimund dans un Compte Rendu de l'<a href="https://fr-m-wikipedia-org.translate.goog/wiki/Acad%C3%A9mie_des_sciences_(France)?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Académie des sciences (France)">Académie des sciences</a><sup id="cite_ref-DeglaciationImpacts2001_3-2" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-DeglaciationImpacts2001-3"><span class="cite_crochet">[</span>3<span class="cite_crochet">]</span></a></sup>.</li> <li>À la suite des modifications différentielles de pression le long de certaines failles, des interactions avec la <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Sismicit%C3%A9?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-redirect" title="Sismicité">sismicité</a> sous-marine, dont réactivation de failles situées sous les fonds marins peuvent accompagner ces phénomènes de rebonds (ex : faille centrale du <a href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Champ_de_Visund&action=edit&redlink=1&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="new" title="Champ de Visund (page inexistante)">champ de Visund</a>, une faille normale inactive d'orientation grossièrement nord–sud, réactivée en jeu inverse dans les derniers 15 000 ans à cause d'un champ de contrainte en compression est–ouest, résultant de la <a href="https://fr-m-wikipedia-org.translate.goog/wiki/D%C3%A9glaciation?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-redirect" title="Déglaciation">déglaciation</a>). <br> Des fuites de gaz profonds peuvent aussi se produire le long de failles en mouvement ou réactivées, phénomènes observés dans le nord de la Mer du Nord par exemple<sup id="cite_ref-FailleReactivation2000_2-1" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-FailleReactivation2000-2"><span class="cite_crochet">[</span>2<span class="cite_crochet">]</span></a></sup> sur une « <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Faille_inverse?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Faille inverse">faille inverse</a> » restée longtemps inactive, à cause d'une <b>« augmentation récente de la contrainte de compression »</b> dans la zone ; associée à un « rebond post-glaciaire » (soulèvement de masses géologiques (émergées ou immergées) à la suite de la fonte de la calotte glaciaire, bien plus rapide en <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Arctique?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Arctique">arctique</a> qu'en <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Antarctique?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Antarctique">antarctique</a>)<sup id="cite_ref-FailleReactivation2000_2-2" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-FailleReactivation2000-2"><span class="cite_crochet">[</span>2<span class="cite_crochet">]</span></a></sup>, mais aussi à une pression interstitielle localement élevée dans la roche (ici en raison de la présence de <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Gaz_naturel?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Gaz naturel">gaz naturel</a> dans un réservoir d'<a href="https://fr-m-wikipedia-org.translate.goog/wiki/Hydrocarbure?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Hydrocarbure">hydrocarbure</a> situé sur le côté d’une des parois de la faille<sup id="cite_ref-FailleReactivation2000_2-3" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-FailleReactivation2000-2"><span class="cite_crochet">[</span>2<span class="cite_crochet">]</span></a></sup>), et ici en raison également d'une orientation de faille favorisant à nouveau son glissement (dans le contexte du champ de contrainte actuelle)<sup id="cite_ref-FailleReactivation2000_2-4" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-FailleReactivation2000-2"><span class="cite_crochet">[</span>2<span class="cite_crochet">]</span></a></sup>.</li> </ul> </section> <div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(2)"> <span class="indicator mf-icon mf-icon-expand mf-icon--small"></span> <h2 id="Indices_géologiques"><span id="Indices_g.C3.A9ologiques"></span>Indices géologiques</h2><span class="mw-editsection"> <a role="button" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&section=3&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Modifier la section : Indices géologiques" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>modifier</span> </a> </span> </div> <section class="mf-section-2 collapsible-block" id="mf-section-2"> <ul> <li>Des témoignages géologiques de ce phénomène peuvent être trouvés, dont les <i>plages fossiles</i> et <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Terrasse_marine?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Terrasse marine">terrasses marines</a> (<span class="citation">« marqueurs de l'interaction entre soulèvement et oscillation du niveau de la mer. »</span><sup id="cite_ref-4" class="reference"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_note-4"><span class="cite_crochet">[</span>4<span class="cite_crochet">]</span></a></sup>).</li> </ul> </section> <div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(3)"> <span class="indicator mf-icon mf-icon-expand mf-icon--small"></span> <h2 id="Références"><span id="R.C3.A9f.C3.A9rences"></span>Références</h2><span class="mw-editsection"> <a role="button" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&section=4&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Modifier la section : Références" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>modifier</span> </a> </span> </div> <section class="mf-section-3 collapsible-block" id="mf-section-3"> <div class="references-small decimal" style=""> <div class="mw-references-wrap"> <ol class="references"> <li id="cite_note-1"><span class="mw-cite-backlink noprint"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-1">↑</a> </span><span class="reference-text"><span class="ouvrage" id="Johansson_et_al.2002"><span class="ouvrage" id="J.M._Johansson_et_al.2002"><abbr class="abbr indicateur-langue" title="Langue : anglais">(en)</abbr> J.M. Johansson et al., « <cite style="font-style:normal" lang="en">Continuous GPS measurements of postglacial adjustment in Fennoscandia. 1. Geodetic results</cite> », <i><span class="lang-en" lang="en">Journal of Geophysical Research</span></i>, <abbr class="abbr" title="volume">vol.</abbr> 107,‎ <time class="nowrap" datetime="2002-08" data-sort-value="2002-08">août 2002</time> <small style="line-height:1em;">(<a href="https://fr-m-wikipedia-org.translate.goog/wiki/Digital_Object_Identifier?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Digital Object Identifier">DOI</a> <span class="plainlinks noarchive nowrap"><a rel="nofollow" class="external text" href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://dx.doi.org/10.1029/2001JB000400">10.1029/2001JB000400</a></span>)</small><span class="Z3988" title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Continuous+GPS+measurements+of+postglacial+adjustment+in+Fennoscandia.+1.+Geodetic+results&rft.jtitle=Journal+of+Geophysical+Research&rft.au=J.M.+Johansson+et+al.&rft.date=2002-08&rft.volume=107&rft_id=info%3Adoi%2F10.1029%2F2001JB000400&rfr_id=info%3Asid%2Ffr.wikipedia.org%3ARebond+post-glaciaire"></span></span></span>.</span></li> <li id="cite_note-FailleReactivation2000-2"><span class="mw-cite-backlink noprint">↑ <sup><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-FailleReactivation2000_2-0">a</a> <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-FailleReactivation2000_2-1">b</a> <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-FailleReactivation2000_2-2">c</a> <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-FailleReactivation2000_2-3">d</a> et <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-FailleReactivation2000_2-4">e</a></sup> </span><span class="reference-text">David Wiprut et Mark D. Zoback, <i>Fault reactivation and fluid flow along a previously dormant normal fault in the northern North Sea</i> ; (<a href="https://fr-m-wikipedia-org.translate.goog/wiki/Universit%C3%A9_Stanford?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Université Stanford">université Stanford</a>), doi: 10.1130/0091-7613(2000) ; 28<595:FRAFFA> ; 2.0.CO;2 v. 28 no. 7 p. 595-598 ; <a rel="nofollow" class="external text" href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=http://geology.gsapubs.org/content/28/7/595.short">Résumé</a></span></li> <li id="cite_note-DeglaciationImpacts2001-3"><span class="mw-cite-backlink noprint">↑ <sup><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-DeglaciationImpacts2001_3-0">a</a> <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-DeglaciationImpacts2001_3-1">b</a> et <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-DeglaciationImpacts2001_3-2">c</a></sup> </span><span class="reference-text">Mark D. Zoback et Balz Grollimund (2001), <i>Impact of deglaciation on present-day intraplate seismicity in eastern North America and western Europe ; Impact de la déglaciation sur la séismicité intra-plaque actuelle dans l'Est de l'Amérique du Nord et en Europe occidentale</i> ; <a href="https://fr-m-wikipedia-org.translate.goog/wiki/Comptes_rendus_hebdomadaires_des_s%C3%A9ances_de_l%27Acad%C3%A9mie_des_sciences?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Comptes rendus hebdomadaires des séances de l'Académie des sciences">Comptes Rendus de l'Académie des Sciences</a> - Series IIA - Earth and Planetary Science, Volume 333, Issue 1, 15 July 2001, Pages 23–33.</span></li> <li id="cite_note-4"><span class="mw-cite-backlink noprint"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Rebond_post-glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB#cite_ref-4">↑</a> </span><span class="reference-text">Regard, V., Pedoja, K., & Saillard, M. (2012). Les terrasses marines, marqueurs de l'interaction entre soulèvement et oscillation du niveau de la mer. <i>Géochronique</i>, 124, 35-37.</span></li> </ol> </div> </div> </section> <div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(4)"> <span class="indicator mf-icon mf-icon-expand mf-icon--small"></span> <h2 id="Voir_aussi">Voir aussi</h2><span class="mw-editsection"> <a role="button" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&section=5&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Modifier la section : Voir aussi" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>modifier</span> </a> </span> </div> <section class="mf-section-4 collapsible-block" id="mf-section-4"> <div class="mw-heading mw-heading3"> <h3 id="Bibliographie">Bibliographie</h3><span class="mw-editsection"> <a role="button" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&section=6&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Modifier la section : Bibliographie" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>modifier</span> </a> </span> </div> <ul> <li>Bouin M.N (1999) <i>Traitement de données GPS en Antarctique: Mouvements crustaux, rebond post-glaciaire, systèmes de référence</i> (Thèse de Doctorat) (<a rel="nofollow" class="external text" href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=http://cat.inist.fr/?aModele%3DafficheN%26cpsidt%3D203219">Notice Inist-CNRS</a>).</li> <li>Guilcher A (1954) Morphologies littorales et sous-marines. coll. Orbis PUF</li> <li>Hagedoorn J.M, Wolf D & Martinec Z (2007) <i>An estimate of global mean sea-level rise inferred from tide-gauge measurements using glacial-isostatic models consistent with the relative sea-level record</i>. Pure and Applied Geophysics, 164(4), 791-818.(<a rel="nofollow" class="external text" href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://link.springer.com/article/10.1007/s00024-007-0186-7">résumé</a>)</li> <li>Le Meur, E. (1996). <i>Spécificité de l'isostasie en contexte glaciaire. Présentation et application d'un modèle de réponse terrestre</i> (Doctoral dissertation).</li> </ul> <div class="mw-heading mw-heading3"> <h3 id="Articles_connexes">Articles connexes</h3><span class="mw-editsection"> <a role="button" href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Rebond_post-glaciaire&action=edit&section=7&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Modifier la section : Articles connexes" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>modifier</span> </a> </span> </div> <div style="column-count:3;margin:.3em 0;" class="colonnes"> <div style="margin:-.3em 0;"> <ul> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Glaciation?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Glaciation">Glaciation</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Isostasie?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Isostasie">Isostasie</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Subsidence_(g%C3%A9ologie)?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Subsidence (géologie)">Subsidence</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/G%C3%A9ologie?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Géologie">Géologie</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Tectonique?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Tectonique">Tectonique</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Niveau_de_la_mer?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Niveau de la mer">Niveau de la mer</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/%C3%89l%C3%A9vation_du_niveau_de_la_mer?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Élévation du niveau de la mer">Élévation du niveau de la mer</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Risque_sismique?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Risque sismique">Risque sismique</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Lithosph%C3%A8re?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Lithosphère">lithosphère</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/w/index.php?title=Viking_Graben&action=edit&redlink=1&_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="new" title="Viking Graben (page inexistante)">Viking Graben</a></li> <li><a href="https://fr-m-wikipedia-org.translate.goog/wiki/D%C3%A9compression_glaciaire?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" class="mw-redirect" title="Décompression glaciaire">Décompression glaciaire</a></li> </ul> </div> </div> <ul id="bandeau-portail" class="bandeau-portail"> <li><span class="bandeau-portail-element"><span class="bandeau-portail-icone"><span class="noviewer" typeof="mw:File"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Portail:Sciences_de_la_Terre_et_de_l%27Univers?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Portail des sciences de la Terre et de l’Univers"> <noscript> <img alt="icône décorative" src="//upload.wikimedia.org/wikipedia/commons/thumb/7/72/Crystal128-browser.svg/24px-Crystal128-browser.svg.png" decoding="async" width="24" height="24" class="mw-file-element" data-file-width="124" data-file-height="125"> </noscript><span class="lazy-image-placeholder" style="width: 24px;height: 24px;" data-src="//upload.wikimedia.org/wikipedia/commons/thumb/7/72/Crystal128-browser.svg/24px-Crystal128-browser.svg.png" data-alt="icône décorative" data-width="24" data-height="24" data-srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/72/Crystal128-browser.svg/36px-Crystal128-browser.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/72/Crystal128-browser.svg/48px-Crystal128-browser.svg.png 2x" data-class="mw-file-element"> </span></a></span></span> <span class="bandeau-portail-texte"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Portail:Sciences_de_la_Terre_et_de_l%27Univers?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Portail:Sciences de la Terre et de l'Univers">Portail des sciences de la Terre et de l’Univers</a></span> </span></li> <li><span class="bandeau-portail-element"><span class="bandeau-portail-icone"><span class="noviewer" typeof="mw:File"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Portail:G%C3%A9od%C3%A9sie_et_g%C3%A9ophysique?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Portail de la géodésie et de la géophysique"> <noscript> <img alt="icône décorative" src="//upload.wikimedia.org/wikipedia/commons/thumb/5/53/Jordens_inre.svg/23px-Jordens_inre.svg.png" decoding="async" width="23" height="24" class="mw-file-element" data-file-width="800" data-file-height="833"> </noscript><span class="lazy-image-placeholder" style="width: 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de la géographie"> <noscript> <img alt="icône décorative" src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e0/Circle-icons-globe.svg/24px-Circle-icons-globe.svg.png" decoding="async" width="24" height="24" class="mw-file-element" data-file-width="512" data-file-height="512"> </noscript><span class="lazy-image-placeholder" style="width: 24px;height: 24px;" data-src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e0/Circle-icons-globe.svg/24px-Circle-icons-globe.svg.png" data-alt="icône décorative" data-width="24" data-height="24" data-srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/e0/Circle-icons-globe.svg/36px-Circle-icons-globe.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/e0/Circle-icons-globe.svg/48px-Circle-icons-globe.svg.png 2x" data-class="mw-file-element"> </span></a></span></span> <span class="bandeau-portail-texte"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Portail:G%C3%A9ographie?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Portail:Géographie">Portail de la géographie</a></span> </span></li> <li><span class="bandeau-portail-element"><span class="bandeau-portail-icone"><span class="noviewer" typeof="mw:File"><a href="https://fr-m-wikipedia-org.translate.goog/wiki/Portail:Maritime?_x_tr_sl=auto&_x_tr_tl=en&_x_tr_hl=en-GB" title="Portail du monde maritime"> <noscript> <img alt="icône décorative" src="//upload.wikimedia.org/wikipedia/commons/thumb/d/d5/Circle-icons-anchor.svg/24px-Circle-icons-anchor.svg.png" decoding="async" width="24" height="24" class="mw-file-element" data-file-width="512" data-file-height="512"> </noscript><span class="lazy-image-placeholder" style="width: 24px;height: 24px;" data-src="//upload.wikimedia.org/wikipedia/commons/thumb/d/d5/Circle-icons-anchor.svg/24px-Circle-icons-anchor.svg.png" data-alt="icône décorative" data-width="24" data-height="24" data-srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/d5/Circle-icons-anchor.svg/36px-Circle-icons-anchor.svg.png 1.5x, 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interwiki-ar mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://ar.wikipedia.org/wiki/%25D8%25A7%25D8%25B1%25D8%25AA%25D8%25AF%25D8%25A7%25D8%25AF_%25D8%25A8%25D8%25B9%25D8%25AF_%25D8%25AC%25D9%2584%25D9%258A%25D8%25AF%25D9%258A" title="ارتداد بعد جليدي – arabe" lang="ar" hreflang="ar" data-title="ارتداد بعد جليدي" data-language-autonym="العربية" data-language-local-name="arabe" class="interlanguage-link-target"><span>العربية</span></a></li> <li class="interlanguage-link interwiki-ca mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://ca.wikipedia.org/wiki/Ajustament_postglacial" title="Ajustament postglacial – catalan" lang="ca" hreflang="ca" data-title="Ajustament postglacial" data-language-autonym="Català" data-language-local-name="catalan" class="interlanguage-link-target"><span>Català</span></a></li> <li class="interlanguage-link interwiki-cs mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://cs.wikipedia.org/wiki/Postglaci%25C3%25A1ln%25C3%25AD_vzestup" title="Postglaciální vzestup – tchèque" lang="cs" hreflang="cs" data-title="Postglaciální vzestup" data-language-autonym="Čeština" data-language-local-name="tchèque" class="interlanguage-link-target"><span>Čeština</span></a></li> <li class="interlanguage-link interwiki-da mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://da.wikipedia.org/wiki/Landh%25C3%25A6vning" title="Landhævning – danois" lang="da" hreflang="da" data-title="Landhævning" data-language-autonym="Dansk" data-language-local-name="danois" class="interlanguage-link-target"><span>Dansk</span></a></li> <li class="interlanguage-link interwiki-de mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://de.wikipedia.org/wiki/Postglaziale_Landhebung" title="Postglaziale Landhebung – allemand" lang="de" hreflang="de" data-title="Postglaziale Landhebung" data-language-autonym="Deutsch" data-language-local-name="allemand" class="interlanguage-link-target"><span>Deutsch</span></a></li> <li class="interlanguage-link interwiki-el mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://el.wikipedia.org/wiki/%25CE%259C%25CE%25B5%25CF%2584%25CE%25B1%25CF%2580%25CE%25B1%25CE%25B3%25CE%25B5%25CF%2584%25CF%258E%25CE%25B4%25CE%25B7%25CF%2582_%25CE%25AC%25CE%25BD%25CE%25BF%25CE%25B4%25CE%25BF%25CF%2582" title="Μεταπαγετώδης άνοδος – grec" lang="el" hreflang="el" data-title="Μεταπαγετώδης άνοδος" data-language-autonym="Ελληνικά" data-language-local-name="grec" class="interlanguage-link-target"><span>Ελληνικά</span></a></li> <li class="interlanguage-link interwiki-en mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://en.wikipedia.org/wiki/Post-glacial_rebound" title="Post-glacial rebound – anglais" lang="en" hreflang="en" data-title="Post-glacial rebound" data-language-autonym="English" data-language-local-name="anglais" class="interlanguage-link-target"><span>English</span></a></li> <li class="interlanguage-link interwiki-es mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://es.wikipedia.org/wiki/Rebote_posglaciar" title="Rebote posglaciar – espagnol" lang="es" hreflang="es" data-title="Rebote posglaciar" data-language-autonym="Español" data-language-local-name="espagnol" class="interlanguage-link-target"><span>Español</span></a></li> <li class="interlanguage-link interwiki-et mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://et.wikipedia.org/wiki/Glatsioisostaasia" title="Glatsioisostaasia – estonien" lang="et" hreflang="et" data-title="Glatsioisostaasia" data-language-autonym="Eesti" data-language-local-name="estonien" class="interlanguage-link-target"><span>Eesti</span></a></li> <li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://fa.wikipedia.org/wiki/%25D8%25A8%25D8%25B1%25D8%25AE%25D8%25A7%25D8%25B3%25D8%25AA_%25D9%25BE%25D8%25B3%25D8%25A7%25DB%258C%25D8%25AE%25DA%2586%25D8%25A7%25D9%2584%25DB%258C" title="برخاست پسایخچالی – persan" lang="fa" hreflang="fa" data-title="برخاست پسایخچالی" data-language-autonym="فارسی" data-language-local-name="persan" class="interlanguage-link-target"><span>فارسی</span></a></li> <li class="interlanguage-link interwiki-id mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://id.wikipedia.org/wiki/Pantulan_pasca-glasial" title="Pantulan pasca-glasial – indonésien" lang="id" hreflang="id" data-title="Pantulan pasca-glasial" data-language-autonym="Bahasa Indonesia" data-language-local-name="indonésien" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li> <li class="interlanguage-link interwiki-is mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://is.wikipedia.org/wiki/Landris" title="Landris – islandais" lang="is" hreflang="is" data-title="Landris" data-language-autonym="Íslenska" data-language-local-name="islandais" class="interlanguage-link-target"><span>Íslenska</span></a></li> <li class="interlanguage-link interwiki-it mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://it.wikipedia.org/wiki/Rimbalzo_post_glaciale" title="Rimbalzo post glaciale – italien" lang="it" hreflang="it" data-title="Rimbalzo post glaciale" data-language-autonym="Italiano" data-language-local-name="italien" class="interlanguage-link-target"><span>Italiano</span></a></li> <li class="interlanguage-link interwiki-ka mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://ka.wikipedia.org/wiki/%25E1%2583%259E%25E1%2583%259D%25E1%2583%25A1%25E1%2583%25A2%25E1%2583%2592%25E1%2583%259A%25E1%2583%2590%25E1%2583%25AA%25E1%2583%2598%25E1%2583%2590%25E1%2583%259A%25E1%2583%25A3%25E1%2583%25A0%25E1%2583%2598_%25E1%2583%25A3%25E1%2583%2599%25E1%2583%25A3%25E1%2583%25A5%25E1%2583%25AA%25E1%2583%2594%25E1%2583%2595%25E1%2583%2590" title="პოსტგლაციალური უკუქცევა – géorgien" lang="ka" hreflang="ka" data-title="პოსტგლაციალური უკუქცევა" data-language-autonym="ქართული" data-language-local-name="géorgien" class="interlanguage-link-target"><span>ქართული</span></a></li> <li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://ko.wikipedia.org/wiki/%25ED%259B%2584%25EB%25B9%2599%25EA%25B8%25B0_%25EB%25B0%2598%25EB%258F%2599" title="후빙기 반동 – coréen" lang="ko" hreflang="ko" data-title="후빙기 반동" data-language-autonym="한국어" data-language-local-name="coréen" class="interlanguage-link-target"><span>한국어</span></a></li> <li class="interlanguage-link interwiki-la mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://la.wikipedia.org/wiki/Repercussus_postglacialis" title="Repercussus postglacialis – latin" lang="la" hreflang="la" data-title="Repercussus postglacialis" data-language-autonym="Latina" data-language-local-name="latin" class="interlanguage-link-target"><span>Latina</span></a></li> <li class="interlanguage-link interwiki-lt mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://lt.wikipedia.org/wiki/Glacioizostazija" title="Glacioizostazija – lituanien" lang="lt" hreflang="lt" data-title="Glacioizostazija" data-language-autonym="Lietuvių" data-language-local-name="lituanien" class="interlanguage-link-target"><span>Lietuvių</span></a></li> <li class="interlanguage-link interwiki-lv mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://lv.wikipedia.org/wiki/Glacioizost%25C4%2581ze" title="Glacioizostāze – letton" lang="lv" hreflang="lv" data-title="Glacioizostāze" data-language-autonym="Latviešu" data-language-local-name="letton" class="interlanguage-link-target"><span>Latviešu</span></a></li> <li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://nl.wikipedia.org/wiki/Postglaciale_opheffing" title="Postglaciale opheffing – néerlandais" lang="nl" hreflang="nl" data-title="Postglaciale opheffing" data-language-autonym="Nederlands" data-language-local-name="néerlandais" class="interlanguage-link-target"><span>Nederlands</span></a></li> <li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://nn.wikipedia.org/wiki/Landheving" title="Landheving – norvégien nynorsk" lang="nn" hreflang="nn" data-title="Landheving" data-language-autonym="Norsk nynorsk" data-language-local-name="norvégien nynorsk" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li> <li class="interlanguage-link interwiki-no mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://no.wikipedia.org/wiki/Postglasial_landhevning" title="Postglasial landhevning – norvégien bokmål" lang="nb" hreflang="nb" data-title="Postglasial landhevning" data-language-autonym="Norsk bokmål" data-language-local-name="norvégien bokmål" class="interlanguage-link-target"><span>Norsk bokmål</span></a></li> <li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://pl.wikipedia.org/wiki/Ruchy_izostatyczne" title="Ruchy izostatyczne – polonais" lang="pl" hreflang="pl" data-title="Ruchy izostatyczne" data-language-autonym="Polski" data-language-local-name="polonais" class="interlanguage-link-target"><span>Polski</span></a></li> <li class="interlanguage-link interwiki-pt mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://pt.wikipedia.org/wiki/Ajuste_p%25C3%25B3s-glacial" title="Ajuste pós-glacial – portugais" lang="pt" hreflang="pt" data-title="Ajuste pós-glacial" data-language-autonym="Português" data-language-local-name="portugais" class="interlanguage-link-target"><span>Português</span></a></li> <li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://ru.wikipedia.org/wiki/%25D0%2593%25D0%25BB%25D1%258F%25D1%2586%25D0%25B8%25D0%25BE%25D0%25B8%25D0%25B7%25D0%25BE%25D1%2581%25D1%2582%25D0%25B0%25D0%25B7%25D0%25B8%25D1%258F" title="Гляциоизостазия – russe" lang="ru" hreflang="ru" data-title="Гляциоизостазия" data-language-autonym="Русский" data-language-local-name="russe" class="interlanguage-link-target"><span>Русский</span></a></li> <li class="interlanguage-link interwiki-sv mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://sv.wikipedia.org/wiki/Postglacial_landh%25C3%25B6jning" title="Postglacial landhöjning – suédois" lang="sv" hreflang="sv" data-title="Postglacial landhöjning" data-language-autonym="Svenska" data-language-local-name="suédois" class="interlanguage-link-target"><span>Svenska</span></a></li> <li class="interlanguage-link interwiki-tr mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://tr.wikipedia.org/wiki/Glasiyoizostazi" title="Glasiyoizostazi – turc" lang="tr" hreflang="tr" data-title="Glasiyoizostazi" data-language-autonym="Türkçe" data-language-local-name="turc" class="interlanguage-link-target"><span>Türkçe</span></a></li> <li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://translate.google.com/website?sl=auto&tl=en&hl=en-GB&u=https://uk.wikipedia.org/wiki/%25D0%259F%25D1%2596%25D1%2581%25D0%25BB%25D1%258F%25D0%25BB%25D1%258C%25D0%25BE%25D0%25B4%25D0%25BE%25D0%25B2%25D0%25B8%25D0%25BA%25D0%25BE%25D0%25B2%25D0%25B8%25D0%25B9_%25D0%25B2%25D1%2596%25D0%25B4%25D1%2581%25D0%25BA%25D0%25BE%25D0%25BA" title="Післяльодовиковий відскок – ukrainien" lang="uk" hreflang="uk" data-title="Післяльодовиковий відскок" data-language-autonym="Українська" data-language-local-name="ukrainien" class="interlanguage-link-target"><span>Українська</span></a></li> </ul> </section> </div> <div class="minerva-footer-logo"> <img src="/static/images/mobile/copyright/wikipedia-wordmark-fr.svg" alt="Wikipédia" width="119" height="18" style="width: 7.4375em; height: 1.125em;"> </div> <ul id="footer-info" class="footer-info hlist hlist-separated"> <li id="footer-info-lastmod">La dernière modification de cette page a été faite le 20 janvier 2024 à 18:18.</li> <li 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