{"id":98,"date":"2015-07-22T15:56:03","date_gmt":"2015-07-22T15:56:03","guid":{"rendered":"http:\/\/airborne.geophysicsgpr.com\/?page_id=98"},"modified":"2017-03-09T15:23:39","modified_gmt":"2017-03-09T15:23:39","slug":"stinger","status":"publish","type":"page","link":"https:\/\/airborne.geophysicsgpr.com\/fr\/techniques\/magnetometrie\/stinger\/","title":{"rendered":"Lev\u00e9 a\u00e9roport\u00e9 (Stinger)"},"content":{"rendered":"<div id=\"pl-98\"  class=\"panel-layout\" ><div id=\"pg-98-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-98-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-98-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"texte-home-right article panel-widget-style panel-widget-style-for-98-0-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h2 class=\"h2resize\">Le lev\u00e9 a\u00e9roport\u00e9 (Stinger)\u00a0se fait avec\u00a0un magn\u00e9tom\u00e8tre a\u00e9roport\u00e9, positionn\u00e9 au bout d\u2019un aiguillon \u00e0 l\u2019avant d\u2019un h\u00e9licopt\u00e8re et est utilis\u00e9e afin de d\u00e9tecter les anomalies magn\u00e9tiques du champ magn\u00e9tique terrestre local.<\/h2>\n<p>\u00a0<\/p>\n<p>Ces anomalies peuvent servir \u00e0 indiquer la pr\u00e9sence de concentrations de min\u00e9raux ferromagn\u00e9tiques \u00e0 l\u2019int\u00e9rieur de la cro\u00fbte terrestre, et permettent la visualisation de la structure g\u00e9ologique de la cro\u00fbte faisant partie du sous-sol, particuli\u00e8rement la g\u00e9om\u00e9trie spatiale du roc et la pr\u00e9sence de failles. Il s\u2019agit d\u2019un outil particuli\u00e8rement utile pour la cartographie g\u00e9ologique dans les endroits o\u00f9 le substratum rocheux est recouvert par du mort-terrain ou par une masse d\u2019eau.<\/p>\n<p>\u00a0<\/p>\n<p>Le principal d\u00e9fi est de soustraire l\u2019influence du champ magn\u00e9tique caus\u00e9 par l\u2019avion, sur les donn\u00e9es mesur\u00e9es par les magn\u00e9tom\u00e8tres.\u00a0Pour ce faire, un magn\u00e9tom\u00e8tre fluxgate trois (3) axes de Barrington est mont\u00e9 \u00e0 la base de chaque magn\u00e9tom\u00e8tre. Les deux magn\u00e9tom\u00e8tres fluxgate mesurent l'orientation et les taux de variation du champ magn\u00e9tique de l'a\u00e9ronef \u00e0 la base de chaque magn\u00e9tom\u00e8tre par rapport au champ magn\u00e9tique de la Terre.<\/p>\n<p>\u00a0<\/p>\n<p>Les coefficients de correction sont par la suite calcul\u00e9s \u00e0 partir d'une figure de m\u00e9rite (FOM) afin de permettre la compensation en temps r\u00e9el \u00e0 l\u2019aide du compensateur magn\u00e9tique ARC500 de RMS. Une compensation \u00e0 posteriori est aussi possible \u00e0 l\u2019aide de logiciel d\u00e9velopp\u00e9 \u00e0 cet effet.<\/p>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>\n<p>Pour plus d'informations, veuillez contacter notre <a style=\"color: #3a5568\" href=\"mailto:info@geophysicsgpr.com\">\u00c9quipe de lev\u00e9 a\u00e9roport\u00e9<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-98-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-98-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-98-1-0-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"1\" ><div class=\"panel-widget-style panel-widget-style-for-98-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-98\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/P1000349_WEB.jpg\" width=\"4608\" height=\"3456\" srcset=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/P1000349_WEB.jpg 4608w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/P1000349_WEB-300x225.jpg 300w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/P1000349_WEB-1024x768.jpg 1024w\" sizes=\"auto, (max-width: 4608px) 100vw, 4608px\" title=\"Airborne_technique_Stinger\" alt=\"Airborne_technique_Stinger\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-98-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-98-1-1-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"2\" ><div class=\"panel-widget-style panel-widget-style-for-98-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-98\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/M11164_RMF_WEB.jpg\" width=\"1500\" height=\"1913\" srcset=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/M11164_RMF_WEB.jpg 1500w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/M11164_RMF_WEB-235x300.jpg 235w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/M11164_RMF_WEB-803x1024.jpg 803w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" title=\"Airborne_technique_Stinger\" alt=\"Airborne_technique_Stinger\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Le lev\u00e9 a\u00e9roport\u00e9 (Stinger)\u00a0se fait avec\u00a0un magn\u00e9tom\u00e8tre a\u00e9roport\u00e9, positionn\u00e9 au bout d\u2019un aiguillon \u00e0 l\u2019avant d\u2019un h\u00e9licopt\u00e8re et est utilis\u00e9e afin de d\u00e9tecter les anomalies magn\u00e9tiques du champ magn\u00e9tique terrestre local.\u00a0Ces anomalies peuvent servir \u00e0 indiquer la pr\u00e9sence de concentrations de min\u00e9raux ferromagn\u00e9tiques \u00e0 l\u2019int\u00e9rieur de la cro\u00fbte terrestre, et permettent la visualisation de la&#8230;  <a href=\"https:\/\/airborne.geophysicsgpr.com\/fr\/techniques\/magnetometrie\/stinger\/\" class=\"more-link\" title=\"Read Lev\u00e9 a\u00e9roport\u00e9 (Stinger)\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":632,"parent":77,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-98","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/98","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/comments?post=98"}],"version-history":[{"count":21,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/98\/revisions"}],"predecessor-version":[{"id":1009,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/98\/revisions\/1009"}],"up":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/77"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media\/632"}],"wp:attachment":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media?parent=98"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}