{"id":37,"date":"2019-06-11T18:52:12","date_gmt":"2019-06-11T17:52:12","guid":{"rendered":"http:\/\/hebergement.u-psud.fr\/MineralogieGEOPS\/?page_id=37"},"modified":"2024-12-21T02:19:20","modified_gmt":"2024-12-21T01:19:20","slug":"micro-thermometrie-des-inclusions-fluides","status":"publish","type":"page","link":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/?page_id=37","title":{"rendered":"Microthermom\u00e9trie des Inclusions Fluides"},"content":{"rendered":"\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p class=\"justify-text\">La plateforme dispose d\u2019une platine r\u00e9frig\u00e9rante et chauffante (-196\u00b0C \u00e0 600\u00b0C) Linkam MDS600 \u00e0 r\u00e9gulation automatis\u00e9e, mont\u00e9e sur un microscope Leica DM2500M et \u00e9quip\u00e9 d\u2019une cam\u00e9ra Qimaging \u2013 Qicam Fast 1394.<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><a href=\"http:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/wp-content\/uploads\/2024\/12\/microthermometrie.jpg\"><img decoding=\"async\" loading=\"lazy\" width=\"242\" height=\"324\" src=\"http:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/wp-content\/uploads\/2024\/12\/microthermometrie.jpg\" alt=\"\" class=\"wp-image-297\" srcset=\"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/wp-content\/uploads\/2024\/12\/microthermometrie.jpg 242w, https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/wp-content\/uploads\/2024\/12\/microthermometrie-224x300.jpg 224w\" sizes=\"(max-width: 242px) 100vw, 242px\" \/><\/a><\/figure><\/div>\n\n\n<h6 class=\"wp-block-heading\">Principe de l\u2019analyse :<\/h6>\n\n\n\n<p class=\"justify-text\">Cette m\u00e9thode d\u2019analyse microthermom\u00e9trique permet de mesurer les temp\u00e9ratures de changements de phases dans une inclusion fluide pi\u00e9g\u00e9e dans un cristal.<\/p>\n\n\n\n<h6 class=\"wp-block-heading\">Analyses r\u00e9alis\u00e9es sur l\u2019instrument :<\/h6>\n\n\n\n<p class=\"justify-text\">Ces mesures permettent de reconstituer, par exemple, la temp\u00e9rature et la salinit\u00e9 du fluide diag\u00e9n\u00e9tique \u00e0 l\u2019origine des cristaux, ou son taux de CO2, CH4. Cette m\u00e9thode est particuli\u00e8rement int\u00e9ressante pour l\u2019\u00e9tude de l\u2019origine des min\u00e9ralisations dans les bassins.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>La plateforme dispose d\u2019une platine r\u00e9frig\u00e9rante et chauffante (-196\u00b0C \u00e0 600\u00b0C) Linkam MDS600 \u00e0 r\u00e9gulation automatis\u00e9e, mont\u00e9e sur un microscope Leica DM2500M et \u00e9quip\u00e9 d\u2019une cam\u00e9ra Qimaging \u2013 Qicam Fast 1394. Principe de l\u2019analyse : Cette m\u00e9thode d\u2019analyse microthermom\u00e9trique permet de mesurer les temp\u00e9ratures de changements de phases dans une inclusion fluide pi\u00e9g\u00e9e dans un &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/?page_id=37\" class=\"more-link\">Continuer la lecture<span class=\"screen-reader-text\"> de &laquo;&nbsp;Microthermom\u00e9trie des Inclusions Fluides&nbsp;&raquo;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=\/wp\/v2\/pages\/37"}],"collection":[{"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=37"}],"version-history":[{"count":7,"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=\/wp\/v2\/pages\/37\/revisions"}],"predecessor-version":[{"id":499,"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=\/wp\/v2\/pages\/37\/revisions\/499"}],"wp:attachment":[{"href":"https:\/\/hebergement.universite-paris-saclay.fr\/MineralogieGEOPS\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=37"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}