{"id":4527,"date":"2024-05-07T08:46:26","date_gmt":"2024-05-07T06:46:26","guid":{"rendered":"https:\/\/ggi-geophysics.com\/mining\/"},"modified":"2025-08-04T07:26:17","modified_gmt":"2025-08-04T05:26:17","slug":"mining","status":"publish","type":"page","link":"https:\/\/ggi-geophysics.com\/en\/mining\/","title":{"rendered":"Mining"},"content":{"rendered":"\n<div class=\"wp-block-stackable-columns alignfull stk-block-columns stk-block stk-f6d97e9\" data-block-id=\"f6d97e9\"><style>.stk-f6d97e9 {margin-bottom:0px !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-f6d97e9-column alignfull\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-a11fd07 stk-block-background stk--has-background-overlay\" data-v=\"4\" data-block-id=\"a11fd07\"><style>.stk-a11fd07 {background-image:url(https:\/\/ggi-geophysics.com\/wp-content\/uploads\/2024\/05\/dumper-truck-driving-in-a-surface-mine-quarry-mi-2023-11-27-04-51-09-utc-scaled.jpg) !important;}.stk-a11fd07-container{min-height:288px !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-a11fd07-container stk--no-background stk--no-padding\"><div class=\"has-text-align-left stk-block-content stk-inner-blocks stk-a11fd07-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-f5fecca\" id=\"mineria\" data-block-id=\"f5fecca\"><style>.stk-f5fecca {margin-top:96px !important;margin-left:159px !important;}.stk-f5fecca .stk-block-heading__text{color:var(--theme-palette-color-6, #F3F5F9) !important;}<\/style><h1 class=\"stk-block-heading__text has-text-color\">Mining<\/h1><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div>\n\n<div class=\"wp-block-stackable-columns alignfull stk-block-columns stk-block stk-c549432 stk-block-background\" data-block-id=\"c549432\"><style>.stk-c549432 {background-color:#68403e !important;margin-bottom:0px !important;}.stk-c549432:before{background-color:#68403e !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-c549432-column alignwide\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-4852287\" data-v=\"4\" data-block-id=\"4852287\"><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-4852287-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-4852287-inner-blocks\">\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-6c0516e\" data-block-id=\"6c0516e\"><style>.stk-6c0516e .stk-block-text__text{font-size:24px !important;color:var(--theme-palette-color-5, #E7EBEE) !important;}@media screen and (max-width:999px){.stk-6c0516e .stk-block-text__text{font-size:24px !important;}}<\/style><p class=\"stk-block-text__text has-text-color\">Without a doubt, mining targets represent one of the greatest challenges for geophysical exploration techniques. The complex structural, geochemical, and mineralogical characteristics are imprinted not only at depth in the deposits themselves, but also in the abrupt topographic relief that commonly accompanies them. Thus, in these objectives, both the lateral resolution achieved by geophysical techniques and the feasibility of incorporating direct observations in steep relief and underground become particularly important. In these scenarios, the greatest geophysical challenge is having geophysical inversion and visualization software appropriate for these conditions.   <\/p><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div>\n\n<div class=\"wp-block-stackable-columns alignfull stk-block-columns stk-block stk-cd47256 stk-block-background\" data-block-id=\"cd47256\"><style>.stk-cd47256 {background-color:#68403e !important;padding-top:80px !important;padding-bottom:80px !important;margin-bottom:0px !important;}.stk-cd47256:before{background-color:#68403e !important;}.stk-cd47256-column{--stk-column-gap:48px !important;row-gap:32px !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-cd47256-column alignwide\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-11145ff\" data-v=\"4\" data-block-id=\"11145ff\"><style>.stk-11145ff-container{margin-top:0px !important;margin-right:0px !important;margin-bottom:0px !important;margin-left:0px !important;display:flex !important;}.stk-11145ff-inner-blocks{justify-content:center !important;}@media screen and (min-width:690px) and (max-width:999px){.stk-11145ff {flex:var(--stk-flex-grow, 1) 1 calc(96.9% - var(--stk-column-gap, 0px) * 0 \/ 1 ) !important;}}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-11145ff-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-11145ff-inner-blocks\">\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-25905ef\" data-block-id=\"25905ef\"><style>.stk-25905ef .stk-block-text__text{font-size:24px !important;color:var(--theme-palette-color-5, #E7EBEE) !important;}@media screen and (max-width:999px){.stk-25905ef .stk-block-text__text{font-size:24px !important;}}<\/style><p class=\"stk-block-text__text has-text-color has-text-align-center-tablet\">GGI&#8217;s research and development team has a long history of experience in the inversion and interpretation of geophysical data for mining targets, highlighting high-resolution aeromagnetic flight data and AGG data inversion software; as well as high-resolution magnetometric resistivity data, electrical logging and seismic refraction and borehole tomography data. Furthermore, current GGI technology can assimilate direct information from exploration drill holes and excavations, both open-pit and underground. <\/p><\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-e2abe0c\" data-v=\"4\" data-block-id=\"e2abe0c\"><style>.stk-e2abe0c-container{margin-top:0px !important;margin-right:0px !important;margin-bottom:0px !important;margin-left:0px !important;}@media screen and (min-width:690px) and (max-width:999px){.stk-e2abe0c {flex:var(--stk-flex-grow, 1) 1 calc(100% - var(--stk-column-gap, 0px) * 0 \/ 1 ) !important;}}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-e2abe0c-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-e2abe0c-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-cd29b9a\" data-block-id=\"cd29b9a\"><style>.stk-cd29b9a .stk-img-wrapper{height:450px !important;}<\/style><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4132\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/goldfields.jpg\" width=\"820\" height=\"1314\" srcset=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/goldfields.jpg 820w, https:\/\/ggi-geophysics.com\/wp-content\/uploads\/goldfields-768x1231.jpg 768w\" sizes=\"auto, (max-width: 820px) 100vw, 820px\" \/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div>\n\n<div class=\"wp-block-stackable-columns alignfull stk-block-columns stk-has-bottom-separator stk-block stk-d748571 stk-block-background\" data-block-id=\"d748571\"><style>.stk-d748571 .stk--block-align-d748571{align-items:flex-start !important;}.stk-d748571 {background-color:#68403e !important;margin-bottom:0px !important;}.stk-d748571:before{background-color:#68403e !important;}.stk-d748571 > .stk-separator__bottom .stk-separator__wrapper{transform:scaleX(1) !important;height:102px !important;}.stk-d748571 > .stk-separator__bottom svg{filter:drop-shadow(25px 10px 30px var(--theme-palette-color-4, #102136)) !important;}<\/style><div class=\"stk-row stk-inner-blocks stk--block-align-d748571 stk-block-content stk-content-align stk-d748571-column alignwide\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-9382677\" data-v=\"4\" data-block-id=\"9382677\"><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-9382677-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-9382677-inner-blocks\">\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-288798a\" data-block-id=\"288798a\"><style>.stk-288798a .stk-block-text__text{font-size:24px !important;color:var(--theme-palette-color-5, #E7EBEE) !important;}@media screen and (max-width:999px){.stk-288798a .stk-block-text__text{font-size:24px !important;}}<\/style><p class=\"stk-block-text__text has-text-color\">As developers of our own software, we can quickly adopt new interpretation methodologies tailored to the needs and circumstances of each stage of mining operations, from greenfields to reduce investment risks to brownfields to maximize profits. <\/p><\/div>\n<\/div><\/div><\/div>\n<\/div><div class=\"stk-separator stk-separator__bottom\"><div class=\"stk-separator__wrapper\"><svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewBox=\"0 0 1600 200\" class=\"stk-separator__layer-1\" preserveAspectRatio=\"none\" aria-hidden=\"true\"><path class=\"wave-3_svg__st2\" d=\"M1413.6 161.4c-157.9 0-338.2-37.7-495.1-67.4-215.6-40.8-328.1-44.6-418.2-41.1S317 73.4 188.4 102-10 136.2-10 136.2v74.2h1620v-68.5s-68.8 19.5-196.4 19.5z\"><\/path><\/svg><\/div><\/div><\/div>\n\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-a05ba6f\" id=\"soluciones\" data-block-id=\"a05ba6f\"><h2 class=\"stk-block-heading__text\">Solutions<\/h2><\/div>\n\n<div class=\"wp-block-stackable-feature stk-block-feature stk-block stk-d6e9bfd is-style-default\" data-v=\"2\" data-block-id=\"d6e9bfd\"><style>.stk-d6e9bfd {--stk-feature-flex-wrap:nowrap !important;}<\/style><div class=\"stk-content-align stk-d6e9bfd-column stk-container stk-d6e9bfd-container stk--no-background stk--no-padding\"><div class=\"stk-inner-blocks stk-block-content stk-row\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-1cf0672\" data-v=\"4\" data-block-id=\"1cf0672\"><style>.stk-1cf0672 {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-1cf0672-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-1cf0672-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-5df726a\" id=\"a-href-https-prueba-ggi-geophysics-com-servicios-data-type-page-data-id-39-inversion-3-d-conjunta-a-de-datos-agg-aeromagneticos-y-gravimetricos\" data-block-id=\"5df726a\"><h3 class=\"stk-block-heading__text\"><a href=\"https:\/\/ggi-geophysics.com\/servicios\/\" data-type=\"page\" data-id=\"39\">3D joint inversion<\/a> of AGG, aeromagnetic and gravity data<\/h3><\/div>\n\n\n\n<div class=\"wp-block-group is-nowrap is-layout-flex wp-container-core-group-is-layout-6c531013 wp-block-group-is-layout-flex\">\n<ul class=\"wp-block-list has-medium-font-size\">\n<li>Three-dimensional joint inversion based on the <a href=\"http:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/2007GL030409\" target=\"_blank\" rel=\"noopener\">cross-gradient<\/a> methodology.<\/li>\n\n\n\n<li>Extension and in-depth monitoring of lineaments expressed on the surface.<\/li>\n\n\n\n<li>Delimitation of host rocks and areas with a high density of fractures and faults.<\/li>\n\n\n\n<li>Detection of intrusive bodies and hydrothermal alteration zones.<\/li>\n<\/ul>\n<\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-32e5f23\" data-v=\"4\" data-block-id=\"32e5f23\"><style>.stk-32e5f23 {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-32e5f23-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-32e5f23-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-94e4034\" data-block-id=\"94e4034\"><style>.stk-94e4034 .stk-img-wrapper{width:90% !important;height:304px !important;}.stk-94e4034 .stk-img-wrapper img{transform:scale(1) !important;object-position:50% 50% !important;}<\/style><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4133\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3D_joint_inversion_mining.jpg\" width=\"442\" height=\"411\"\/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n\n<div class=\"wp-block-stackable-divider stk-block-divider stk-block stk-3b43a96\" data-block-id=\"3b43a96\"><style>.stk-3b43a96 hr.stk-block-divider__hr{width:100% !important;}<\/style><hr class=\"stk-block-divider__hr\"\/><\/div>\n\n<div class=\"wp-block-stackable-feature stk-block-feature stk-block stk-96d2d75 is-style-default\" data-v=\"2\" data-block-id=\"96d2d75\"><style>.stk-96d2d75 {--stk-feature-flex-wrap:nowrap !important;}<\/style><div class=\"stk-content-align stk-96d2d75-column stk-container stk-96d2d75-container stk--no-background stk--no-padding\"><div class=\"stk-inner-blocks stk-block-content stk-row\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-8e5a230\" data-v=\"4\" data-block-id=\"8e5a230\"><style>.stk-8e5a230 {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-8e5a230-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-8e5a230-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-dee9cc8\" id=\"a-href-https-prueba-ggi-geophysics-com-servicios-data-type-page-data-id-39-inversion-3-d-a-de-datos-de-resistividad-magnetometrica-y-perfiles-ert-en-mineria\" data-block-id=\"dee9cc8\"><h3 class=\"stk-block-heading__text\"><a href=\"https:\/\/ggi-geophysics.com\/servicios\/\" data-type=\"page\" data-id=\"39\">3D inversion<\/a> of magnetometric resistivity data and ERT profiles in mining<\/h3><\/div>\n\n\n\n<div class=\"wp-block-group is-nowrap is-layout-flex wp-container-core-group-is-layout-6c531013 wp-block-group-is-layout-flex\">\n<ul class=\"wp-block-list has-medium-font-size\">\n<li>Three-dimensional inversion based on the finite element method.<\/li>\n\n\n\n<li>High-resolution lateral resistivity variation mapping for the identification of faults, fractures and mineralized zones.<\/li>\n\n\n\n<li>Detection of the presence of water and monitoring of groundwater flow channels.<\/li>\n<\/ul>\n<\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-87824b2\" data-v=\"4\" data-block-id=\"87824b2\"><style>.stk-87824b2 {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-87824b2-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-87824b2-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-c332606\" data-block-id=\"c332606\"><style>.stk-c332606 .stk-img-wrapper{width:100% !important;height:381px !important;}.stk-c332606 .stk-img-wrapper img{transform:scale(0.75) !important;object-position:51% 22% !important;}<\/style><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4134\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion_mmr.jpg\" width=\"1044\" height=\"1279\" srcset=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion_mmr.jpg 1044w, https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion_mmr-768x941.jpg 768w\" sizes=\"auto, (max-width: 1044px) 100vw, 1044px\" \/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n\n<div class=\"wp-block-stackable-divider stk-block-divider stk-block stk-bf38798 stk-block-background\" data-block-id=\"bf38798\"><style>.stk-bf38798 hr.stk-block-divider__hr{width:100% !important;}.stk-bf38798 {background-color:var(--theme-palette-color-8, #ffffff) !important;}.stk-bf38798:before{background-color:var(--theme-palette-color-8, #ffffff) !important;}<\/style><hr class=\"stk-block-divider__hr\"\/><\/div>\n\n<div class=\"wp-block-stackable-feature stk-block-feature stk-block stk-bea2011 is-style-default\" data-v=\"2\" data-block-id=\"bea2011\"><style>.stk-bea2011 {--stk-feature-flex-wrap:nowrap !important;}<\/style><div class=\"stk-content-align stk-bea2011-column stk-container stk-bea2011-container stk--no-background stk--no-padding\"><div class=\"stk-inner-blocks stk-block-content stk-row\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-fac44c4\" data-v=\"4\" data-block-id=\"fac44c4\"><style>.stk-fac44c4 {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-fac44c4-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-fac44c4-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-3d2f71a\" id=\"a-href-https-prueba-ggi-geophysics-com-servicios-data-type-page-data-id-39-inversion-2-d-conjunta-a-de-datos-electricos-potenciales-sismicos-litologia-de-pozos-y-barrenos\" data-block-id=\"3d2f71a\"><h3 class=\"stk-block-heading__text\"><a href=\"https:\/\/ggi-geophysics.com\/servicios\/\" data-type=\"page\" data-id=\"39\">Joint 2D inversion<\/a> of electrical, potential, seismic, well and borehole lithology data<\/h3><\/div>\n\n\n\n<div class=\"wp-block-group is-nowrap is-layout-flex wp-container-core-group-is-layout-6c531013 wp-block-group-is-layout-flex\">\n<ul class=\"wp-block-list has-medium-font-size\">\n<li>Two-dimensional joint inversion based on the <a href=\"http:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2007GL030409\" target=\"_blank\" rel=\"noopener\">cross-gradient<\/a> methodology.<\/li>\n\n\n\n<li><a href=\"http:\/\/doi.org\/10.1130\/G32817.1\" target=\"_blank\" rel=\"noopener\">Integrated interpretation of geological structures<\/a>, lineaments, intrusive bodies, alteration zones, and lithologies based on the combination of multiple physical properties.<\/li>\n<\/ul>\n<\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-4cc4c6b\" data-v=\"4\" data-block-id=\"4cc4c6b\"><style>.stk-4cc4c6b {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-4cc4c6b-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-4cc4c6b-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-2276723\" data-block-id=\"2276723\"><style>.stk-2276723 .stk-img-wrapper{width:442px !important;}<\/style><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4135\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/joint_inversion_mining.jpg\" width=\"710\" height=\"318\" alt=\"Joint inversion in mining\"\/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n\n<div class=\"wp-block-stackable-separator alignfull stk-block-separator stk--no-padding stk-block stk-49404e6 stk-block-background stk--has-background-overlay\" data-block-id=\"49404e6\"><style>.stk-49404e6 {background-image:url(https:\/\/ggi-geophysics.com\/wp-content\/uploads\/aerial-view-of-truck-excavator-in-open-sand-quarry-2025-03-18-15-27-50-utc-scaled.jpg) !important;background-attachment:fixed !important;}<\/style><div class=\"stk-block-separator__inner\"><svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewBox=\"0 0 1600 200\" class=\"stk-separator__layer-1\" preserveAspectRatio=\"none\" aria-hidden=\"true\"><path class=\"wave-2_svg__st2\" d=\"M1432.2 67.4c-88.8-16.7-156-5.3-204 8.5s-147.1 62.2-223.1 73.9c-75.4 11.6-164-7.5-275-27.9S571 88.1 456 98.1c-119.7 10.4-224.7 52-294.4 73-94.5 28.5-171.6-3-171.6-3V210h1620V91.6c-53 10-86.8-7.1-177.8-24.2z\"><\/path><\/svg><\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Mining Without a doubt, mining targets represent one of the greatest challenges for geophysical exploration techniques. The complex structural, geochemical, and mineralogical characteristics are imprinted not only at depth in the deposits themselves, but also in the abrupt topographic relief that commonly accompanies them. Thus, in these objectives, both the lateral resolution achieved by geophysical [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-4527","page","type-page","status-publish","hentry"],"blocksy_meta":{"vertical_spacing_source":"custom","content_area_spacing":"none","has_hero_section":"disabled","styles_descriptor":{"styles":{"desktop":"","tablet":"","mobile":""},"google_fonts":[],"version":6}},"_links":{"self":[{"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages\/4527","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/comments?post=4527"}],"version-history":[{"count":3,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages\/4527\/revisions"}],"predecessor-version":[{"id":4532,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages\/4527\/revisions\/4532"}],"wp:attachment":[{"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/media?parent=4527"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}