{"version":"1.0","provider_name":"Sahel lib","provider_url":"https:\/\/sahellib.org","author_name":"Sahellib","author_url":"https:\/\/sahellib.org\/index.php\/author\/sahellib\/","title":"Contribution des mesures AMS \u00e0 la compr\u00e9hension des terrains migmatitiques de Pointe G\u00e9ologie, Terre Ad\u00e9lie (Antarctique oriental) - Sahel lib","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"mLBqucor80\"><a href=\"https:\/\/sahellib.org\/index.php\/docs\/docly-documentation\/code\/code-default-theme\/\">Contribution des mesures AMS \u00e0 la compr\u00e9hension des terrains migmatitiques de Pointe G\u00e9ologie, Terre Ad\u00e9lie (Antarctique oriental)<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/sahellib.org\/index.php\/docs\/docly-documentation\/code\/code-default-theme\/embed\/#?secret=mLBqucor80\" width=\"600\" height=\"338\" title=\"\u00ab\u00a0Contribution des mesures AMS \u00e0 la compr\u00e9hension des terrains migmatitiques de Pointe G\u00e9ologie, Terre Ad\u00e9lie (Antarctique oriental)\u00a0\u00bb &#8212; Sahel lib\" data-secret=\"mLBqucor80\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\n\/*! This file is auto-generated *\/\n!function(d,l){\"use strict\";l.querySelector&&d.addEventListener&&\"undefined\"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!\/[^a-zA-Z0-9]\/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret=\"'+t.secret+'\"]'),o=l.querySelectorAll('blockquote[data-secret=\"'+t.secret+'\"]'),c=new RegExp(\"^https?:$\",\"i\"),i=0;i<o.length;i++)o[i].style.display=\"none\";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute(\"style\"),\"height\"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):\"link\"===t.message&&(r=new URL(s.getAttribute(\"src\")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener(\"message\",d.wp.receiveEmbedMessage,!1),l.addEventListener(\"DOMContentLoaded\",function(){for(var e,t,s=l.querySelectorAll(\"iframe.wp-embedded-content\"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute(\"data-secret\"))||(t=Math.random().toString(36).substring(2,12),e.src+=\"#?secret=\"+t,e.setAttribute(\"data-secret\",t)),e.contentWindow.postMessage({message:\"ready\",secret:t},\"*\")},!1)))}(window,document);\n\/\/# sourceURL=https:\/\/sahellib.org\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","description":"Points forts Pointe G\u00e9ologie a connu un \u00e9v\u00e9nement anatectique intense durant le Pal\u00e9oprot\u00e9rozo\u00efque. Les m\u00e9lanosomes, les leucosomes felsiques et les anatexites d\u00e9veloppent des signatures AMS contrast\u00e9es. Les r\u00e9sultats mettent en \u00e9vidence le r\u00f4le de la remont\u00e9e magmatique induite par la gravit\u00e9. Abstrait Une cartographie magn\u00e9tique d\u00e9taill\u00e9e, utilisant la technique&nbsp;d&#8217;anisotropie de susceptibilit\u00e9 magn\u00e9tique&nbsp;(ASM), a \u00e9t\u00e9 r\u00e9alis\u00e9e [&hellip;]"}