{"id":4523,"date":"2024-05-07T08:46:26","date_gmt":"2024-05-07T06:46:26","guid":{"rendered":"https:\/\/ggi-geophysics.com\/geothermal-energy\/"},"modified":"2025-08-03T07:59:17","modified_gmt":"2025-08-03T05:59:17","slug":"geothermal-energy","status":"publish","type":"page","link":"https:\/\/ggi-geophysics.com\/en\/geothermal-energy\/","title":{"rendered":"Geothermal Energy"},"content":{"rendered":"\n<div class=\"wp-block-stackable-columns alignfull stk-block-columns stk-block stk-c2a98d6 stk-block-background\" data-block-id=\"c2a98d6\"><style>.stk-c2a98d6 {min-height:0px !important;align-items:center !important;padding-top:0px !important;padding-right:0px !important;padding-bottom:0px !important;padding-left:0px !important;margin-top:-200px !important;margin-bottom:0px !important;display:flex !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-c2a98d6-column alignfull\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-52c2018 stk-block-background stk--has-background-overlay\" data-v=\"4\" data-block-id=\"52c2018\"><style>.stk-52c2018 {background-image:url(https:\/\/ggi-geophysics.com\/wp-content\/uploads\/2024\/05\/panoramic-view-of-old-faithful-geyser-at-colorful-2023-11-27-05-26-10-utc-1-scaled.jpg) !important;min-height:0px !important;}.stk-52c2018-container{min-height:507px !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-52c2018-container stk--no-background stk--no-padding\"><div class=\"has-text-align-center stk-block-content stk-inner-blocks stk-52c2018-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-7f0ed63\" id=\"geotermia\" data-block-id=\"7f0ed63\"><style>.stk-7f0ed63 {max-width:1067px !important;min-width:auto !important;margin-top:200px !important;margin-left:-200px !important;}.stk-7f0ed63 .stk-block-heading__text{font-size:52px !important;color:#ffffff !important;}@media screen and (max-width:999px){.stk-7f0ed63 .stk-block-heading__text{font-size:50px !important;}}@media screen and (max-width:689px){.stk-7f0ed63 {margin-top:200px !important;margin-right:8px !important;margin-left:-3px !important;}}<\/style><h1 class=\"stk-block-heading__text has-text-color has-text-align-center\">Geothermal Energy<\/h1><\/div>\n\n\n\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-b6beb98\" data-block-id=\"b6beb98\"><style>.stk-b6beb98 {margin-bottom:21px !important;}<\/style><p class=\"stk-block-text__text has-text-align-center\"><\/p><\/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-1ef99ef stk-block-background stk--has-background-overlay\" data-block-id=\"1ef99ef\"><style>.stk-1ef99ef {background-color:linear-gradient(180deg,rgb(209,143,120) 0%,rgb(244,222,169) 100%) !important;}.stk-1ef99ef:before{background-image:linear-gradient(180deg,rgb(209,143,120) 0%,rgb(244,222,169) 100%) !important;}.stk-1ef99ef > .stk-separator__bottom{z-index:6 !important;}.stk-1ef99ef > .stk-separator__bottom .stk-separator__wrapper{height:102px !important;}.stk-1ef99ef > .stk-separator__bottom svg{filter:drop-shadow(2px 4px 6px #000) !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-1ef99ef-column alignwide\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-9dea6fd\" data-v=\"4\" data-block-id=\"9dea6fd\"><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-9dea6fd-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-9dea6fd-inner-blocks\">\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-bc62114\" data-block-id=\"bc62114\"><style>.stk-bc62114 .stk-block-text__text{font-size:24px !important;color:var(--theme-palette-color-4, #102136) !important;}@media screen and (max-width:999px){.stk-bc62114 .stk-block-text__text{font-size:24px !important;}}<\/style><p class=\"stk-block-text__text has-text-color\">In a society with increasing energy consumption, geothermal energy plays a fundamental role among renewable alternatives, harnessing the Earth&#8217;s internal heat to generate continuous electrical energy. Geophysical methodologies are one of the best tools for identifying and assessing the availability of these geothermal resources in great detail.<\/p><\/div>\n\n\n\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-d8d2b54\" data-block-id=\"d8d2b54\"><style>.stk-d8d2b54 .stk-block-text__text{font-size:24px !important;color:var(--theme-palette-color-4, #102136) !important;}@media screen and (max-width:999px){.stk-d8d2b54 .stk-block-text__text{font-size:24px !important;}}<\/style><p class=\"stk-block-text__text has-text-color\">At GGI, we develop and apply unique methodologies that transform your MT, TEM, SEVS, magnetic, gravity and seismic data into high-resolution three- and two-dimensional models to provide greater certainty in identifying geothermally relevant features of the geological environment, including:<\/p><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-9df07bf\" data-block-id=\"9df07bf\"><div class=\"stk-row stk-inner-blocks stk-block-content\">\n<div class=\"wp-block-stackable-icon stk-block-icon has-text-align-left stk-block stk-713d5ed\" data-block-id=\"713d5ed\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-713d5ed\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-713-d-5-ed-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-713-d-5-ed-color-2)\"><\/stop><\/lineargradient><\/defs><\/svg><svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewbox=\"0 0 512 512\" aria-hidden=\"true\" width=\"32\" height=\"32\"><path d=\"M256 512A256 256 0 1 0 256 0a256 256 0 1 0 0 512zM369 209L241 337c-9.4 9.4-24.6 9.4-33.9 0l-64-64c-9.4-9.4-9.4-24.6 0-33.9s24.6-9.4 33.9 0l47 47L335 175c9.4-9.4 24.6-9.4 33.9 0s9.4 24.6 0 33.9z\"><\/path><\/svg><\/div><\/span><\/div>\n\n\n\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-a25e0b1\" id=\"delimitacion-tridimensional-de-cuencas-y-reservorios-geotermicos\" data-block-id=\"a25e0b1\"><style>.stk-a25e0b1 .stk-block-heading__text{font-size:24px !important;}@media screen and (max-width:999px){.stk-a25e0b1 .stk-block-heading__text{font-size:24px !important;}}<\/style><h3 class=\"stk-block-heading__text\">Three-dimensional delimitation of geothermal basins and reservoirs.<\/h3><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-d3b0550\" data-block-id=\"d3b0550\"><div class=\"stk-row stk-inner-blocks stk-block-content\">\n<div class=\"wp-block-stackable-icon stk-block-icon has-text-align-left stk-block stk-004b3bd\" data-block-id=\"004b3bd\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-004b3bd\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-004-b-3-bd-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-004-b-3-bd-color-2)\"><\/stop><\/lineargradient><\/defs><\/svg><svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewbox=\"0 0 512 512\" aria-hidden=\"true\" width=\"32\" height=\"32\"><path d=\"M256 512A256 256 0 1 0 256 0a256 256 0 1 0 0 512zM369 209L241 337c-9.4 9.4-24.6 9.4-33.9 0l-64-64c-9.4-9.4-9.4-24.6 0-33.9s24.6-9.4 33.9 0l47 47L335 175c9.4-9.4 24.6-9.4 33.9 0s9.4 24.6 0 33.9z\"><\/path><\/svg><\/div><\/span><\/div>\n\n\n\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-841f7db\" id=\"caracterizacion-geofisica-del-reservorio-y-rocas-encajonantes\" data-block-id=\"841f7db\"><style>.stk-841f7db .stk-block-heading__text{font-size:24px !important;}@media screen and (max-width:999px){.stk-841f7db .stk-block-heading__text{font-size:24px !important;}}<\/style><h3 class=\"stk-block-heading__text\">Geophysical characterization of the reservoir and host rocks.<\/h3><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-8267157\" data-block-id=\"8267157\"><div class=\"stk-row stk-inner-blocks stk-block-content\">\n<div class=\"wp-block-stackable-icon stk-block-icon has-text-align-left stk-block stk-e89d714\" data-block-id=\"e89d714\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-e89d714\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-e-89-d-714-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-e-89-d-714-color-2)\"><\/stop><\/lineargradient><\/defs><\/svg><svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewbox=\"0 0 512 512\" aria-hidden=\"true\" width=\"32\" height=\"32\"><path d=\"M256 512A256 256 0 1 0 256 0a256 256 0 1 0 0 512zM369 209L241 337c-9.4 9.4-24.6 9.4-33.9 0l-64-64c-9.4-9.4-9.4-24.6 0-33.9s24.6-9.4 33.9 0l47 47L335 175c9.4-9.4 24.6-9.4 33.9 0s9.4 24.6 0 33.9z\"><\/path><\/svg><\/div><\/span><\/div>\n\n\n\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-2f9fe9b\" id=\"localizacion-de-zonas-con-potencial-geotermico\" data-block-id=\"2f9fe9b\"><style>.stk-2f9fe9b .stk-block-heading__text{font-size:24px !important;}@media screen and (max-width:999px){.stk-2f9fe9b .stk-block-heading__text{font-size:24px !important;}}<\/style><h3 class=\"stk-block-heading__text\">Location of areas with geothermal potential.<\/h3><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-99e93db\" data-block-id=\"99e93db\"><div class=\"stk-row stk-inner-blocks stk-block-content\">\n<div class=\"wp-block-stackable-icon stk-block-icon has-text-align-left stk-block stk-21c98c6\" data-block-id=\"21c98c6\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-21c98c6\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-21-c-98-c-6-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-21-c-98-c-6-color-2)\"><\/stop><\/lineargradient><\/defs><\/svg><svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewbox=\"0 0 512 512\" aria-hidden=\"true\" width=\"32\" height=\"32\"><path d=\"M256 512A256 256 0 1 0 256 0a256 256 0 1 0 0 512zM369 209L241 337c-9.4 9.4-24.6 9.4-33.9 0l-64-64c-9.4-9.4-9.4-24.6 0-33.9s24.6-9.4 33.9 0l47 47L335 175c9.4-9.4 24.6-9.4 33.9 0s9.4 24.6 0 33.9z\"><\/path><\/svg><\/div><\/span><\/div>\n\n\n\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-9a3c512\" id=\"identificacion-de-lineamientos-estructurales\" data-block-id=\"9a3c512\"><style>.stk-9a3c512 .stk-block-heading__text{font-size:24px !important;}@media screen and (max-width:999px){.stk-9a3c512 .stk-block-heading__text{font-size:24px !important;}}<\/style><h3 class=\"stk-block-heading__text\">Identification of structural lineaments.<\/h3><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-93fac7f\" data-block-id=\"93fac7f\"><div class=\"stk-row stk-inner-blocks stk-block-content\">\n<div class=\"wp-block-stackable-icon stk-block-icon has-text-align-left stk-block stk-501ac33\" data-block-id=\"501ac33\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-501ac33\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-501-ac-33-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-501-ac-33-color-2)\"><\/stop><\/lineargradient><\/defs><\/svg><svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewbox=\"0 0 512 512\" aria-hidden=\"true\" width=\"32\" height=\"32\"><path d=\"M256 512A256 256 0 1 0 256 0a256 256 0 1 0 0 512zM369 209L241 337c-9.4 9.4-24.6 9.4-33.9 0l-64-64c-9.4-9.4-9.4-24.6 0-33.9s24.6-9.4 33.9 0l47 47L335 175c9.4-9.4 24.6-9.4 33.9 0s9.4 24.6 0 33.9z\"><\/path><\/svg><\/div><\/span><\/div>\n\n\n\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-0dccd0d\" id=\"discriminacion-de-diferentes-reservorios-y-unidades-geologicas\" data-block-id=\"0dccd0d\"><style>.stk-0dccd0d .stk-block-heading__text{font-size:24px !important;}@media screen and (max-width:999px){.stk-0dccd0d .stk-block-heading__text{font-size:24px !important;}}<\/style><h3 class=\"stk-block-heading__text\">Discrimination of different reservoirs and geological units.<\/h3><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-8b3b207\" data-block-id=\"8b3b207\"><style>.stk-8b3b207 .stk-block-text__text{font-size:24px !important;color:var(--theme-palette-color-4, #102136) !important;}@media screen and (max-width:999px){.stk-8b3b207 .stk-block-text__text{font-size:24px !important;}}<\/style><p class=\"stk-block-text__text has-text-color\">All of this provides comprehensive support for establishing both conceptual geothermal models in the exploratory stages and reservoir models in operating geothermal fields. <\/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 d=\"M-10 210h1620V105.2H-10z\"><\/path><\/svg><\/div><\/div><\/div>\n\n<div class=\"wp-block-stackable-columns alignwide stk-block-columns stk-block stk-19dc9cb\" data-block-id=\"19dc9cb\"><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-19dc9cb-column alignwide\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-c68a0f7\" data-v=\"4\" data-block-id=\"c68a0f7\"><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-c68a0f7-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-c68a0f7-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-d2c0b54 stk-block-background stk--has-background-overlay\" id=\"soluciones\" data-block-id=\"d2c0b54\"><style>.stk-d2c0b54 {background-color:transparent !important;}.stk-d2c0b54:before{background-image:linear-gradient(90deg,  0%, rgba(0,0,0,0) 100%) !important;}<\/style><h2 class=\"stk-block-heading__text has-text-align-center\">Solutions<\/h2><\/div>\n\n\n\n<div class=\"wp-block-stackable-feature stk-block-feature stk-block stk-fd637c0 stk-block-background is-style-default\" data-v=\"2\" data-block-id=\"fd637c0\"><style>.stk-fd637c0 {--stk-feature-flex-wrap:nowrap !important;background-color:#cec1b3 !important;overflow:hidden !important;box-shadow:0px 5px 30px -10px var(--theme-palette-color-3, #4d5d6d) !important;border-style:solid !important;border-top-width:0px !important;border-right-width:0px !important;border-bottom-width:0px !important;border-left-width:0px !important;}.stk-fd637c0:before{background-color:#cec1b3 !important;}<\/style><div class=\"stk-content-align stk-fd637c0-column stk-container stk-fd637c0-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-714e0cb\" data-v=\"4\" data-block-id=\"714e0cb\"><style>.stk-714e0cb {align-self:center !important;}@media screen and (min-width:690px){.stk-714e0cb {flex:var(--stk-flex-grow, 1) 1 calc(50% - var(--stk-column-gap, 0px) * 1 \/ 2 ) !important;}}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-714e0cb-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-714e0cb-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-c9304df\" id=\"a-href-https-prueba-ggi-geophysics-com-servicios-data-type-page-data-id-39-inversion-3-d-a-de-datos-amt-mt-en-geotermia\" data-block-id=\"c9304df\"><h3 class=\"stk-block-heading__text\"><a href=\"https:\/\/ggi-geophysics.com\/servicios\/\" data-type=\"page\" data-id=\"39\">3D inversion<\/a> of AMT\/MT 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\">\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-88b31045055dd1aa1622048423795ec2\">Three-dimensional inversion of MT data (apparent resistivity, phase and tipper) based on the finite element method.<\/li>\n\n\n\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-cf8b3fb7489537e1d33c333d43909713\">Interpretation of 3D models for the identification of structural lineaments as well as shallow and deep reservoirs.<\/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-d96c170\" data-v=\"4\" data-block-id=\"d96c170\"><style>.stk-d96c170 {align-self:center !important;}@media screen and (min-width:690px){.stk-d96c170 {flex:var(--stk-flex-grow, 1) 1 calc(50% - var(--stk-column-gap, 0px) * 1 \/ 2 ) !important;}}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-d96c170-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-d96c170-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-9c40709\" data-block-id=\"9c40709\"><style>.stk-9c40709 {overflow:hidden !important;}<\/style><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4209\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion_mt.jpg\" width=\"791\" height=\"486\" srcset=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion_mt.jpg 791w, https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion_mt-768x472.jpg 768w\" sizes=\"auto, (max-width: 791px) 100vw, 791px\" \/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-feature stk-block-feature stk-block stk-e7cfafc stk-block-background is-style-default\" data-v=\"2\" data-block-id=\"e7cfafc\"><style>.stk-e7cfafc {--stk-feature-flex-wrap:nowrap !important;background-color:#cec1b3 !important;overflow:hidden !important;box-shadow:0px 5px 30px -10px var(--theme-palette-color-3, #4d5d6d) !important;border-top-width:1px !important;border-right-width:1px !important;border-bottom-width:1px !important;border-left-width:1px !important;}.stk-e7cfafc:before{background-color:#cec1b3 !important;}<\/style><div class=\"stk-content-align stk-e7cfafc-column stk-container stk-e7cfafc-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-5009770\" data-v=\"4\" data-block-id=\"5009770\"><style>.stk-5009770 {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-5009770-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-5009770-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-7aa7557\" id=\"a-href-https-prueba-ggi-geophysics-com-servicios-data-type-page-data-id-39-inversion-conjunta-2-d-a-con-cross-gradients-en-geotermia\" data-block-id=\"7aa7557\"><style>.stk-7aa7557 .stk-block-heading__text{color:var(--theme-palette-color-4, #102136) !important;}<\/style><h3 class=\"stk-block-heading__text has-text-color\"><a href=\"https:\/\/ggi-geophysics.com\/servicios\/\" data-type=\"page\" data-id=\"39\">Two-dimensional cross-gradient joint inversion<\/a> in geothermal applications<\/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\">\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-1848f1fc00622e90c59ac7f1f22ae0e0\">Two-dimensional <a href=\"http:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2007GL030409\" target=\"_blank\" rel=\"noopener\">cross-gradient <\/a>joint inversion of MT, DC, gravity, magnetic, seismic and well log data.<\/li>\n\n\n\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-e1dadef1f805a69863c6971db0155517\">Identification of geological units and their associated characteristics, both in the mineral and fluid phases, using images of multiple physical properties (geospectral images).<\/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-244606a\" data-v=\"4\" data-block-id=\"244606a\"><style>.stk-244606a {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-244606a-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-244606a-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-12f0046\" data-block-id=\"12f0046\"><style>.stk-12f0046 .stk-img-wrapper{width:509px !important;}<\/style><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4125\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/joint_MT_gravity.jpg\" width=\"790\" height=\"527\" alt=\"Geothermal Energy\" srcset=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/joint_MT_gravity.jpg 790w, https:\/\/ggi-geophysics.com\/wp-content\/uploads\/joint_MT_gravity-768x512.jpg 768w\" sizes=\"auto, (max-width: 790px) 100vw, 790px\" \/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-feature stk-block-feature stk-block stk-057b035 stk-block-background is-style-default\" data-v=\"2\" data-block-id=\"057b035\"><style>.stk-057b035 {--stk-feature-flex-wrap:nowrap !important;background-color:#cec1b3 !important;overflow:hidden !important;box-shadow:0px 5px 30px -10px var(--theme-palette-color-3, #4d5d6d) !important;}.stk-057b035:before{background-color:#cec1b3 !important;}<\/style><div class=\"stk-content-align stk-057b035-column stk-container stk-057b035-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-5a1fb8a\" data-v=\"4\" data-block-id=\"5a1fb8a\"><style>.stk-5a1fb8a {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-5a1fb8a-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-5a1fb8a-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-b5ce8fe\" id=\"a-href-https-prueba-ggi-geophysics-com-servicios-data-type-page-data-id-39-inversion-conjunta-3-d-a-de-datos-rmm-y-amt-mt\" data-block-id=\"b5ce8fe\"><h3 class=\"stk-block-heading__text\"><a href=\"https:\/\/ggi-geophysics.com\/servicios\/\" data-type=\"page\" data-id=\"39\">3D joint inversion<\/a> of MMR and AMT\/MT 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\">\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-b09c0bfe75bb8e2e1b2edd5a05fdd414\">Three-dimensional joint inversion of magnetotelluric and magnetometric resistivity data based on the finite element method.<\/li>\n\n\n\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-ddacba61af66f33b801820603e3fbd4f\">Interpretation of high lateral resolution resistivity models at depths less than 1 km for detailed delineation of shallow reservoirs and fluid upwelling 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-553cbde\" data-v=\"4\" data-block-id=\"553cbde\"><style>.stk-553cbde {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-553cbde-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-553cbde-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-d85b337\" data-block-id=\"d85b337\"><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4127\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion-mmr-MT.jpg\" width=\"1263\" height=\"1098\" srcset=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion-mmr-MT.jpg 1263w, https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3d_inversion-mmr-MT-768x668.jpg 768w\" sizes=\"auto, (max-width: 1263px) 100vw, 1263px\" \/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-feature stk-block-feature stk-block stk-b2a5470 stk-block-background is-style-default\" data-v=\"2\" data-block-id=\"b2a5470\"><style>.stk-b2a5470 {--stk-feature-flex-wrap:nowrap !important;background-color:#cec1b3 !important;border-top-left-radius:0px !important;border-top-right-radius:0px !important;border-bottom-right-radius:0px !important;border-bottom-left-radius:0px !important;overflow:hidden !important;box-shadow:0px 5px 30px -10px var(--theme-palette-color-3, #4d5d6d) !important;}.stk-b2a5470:before{background-color:#cec1b3 !important;}<\/style><div class=\"stk-content-align stk-b2a5470-column stk-container stk-b2a5470-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-594bbab\" data-v=\"4\" data-block-id=\"594bbab\"><style>.stk-594bbab {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-594bbab-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-594bbab-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-de97c37\" id=\"inversion-conjunta-3-d-de-datos-gravimetricos-y-magneticos\" data-block-id=\"de97c37\"><h3 class=\"stk-block-heading__text\">3D joint inversion of gravity and magnetic 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\">\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-648e97754fd70609df5e82dc90aa0aec\">Three-dimensional <a href=\"http:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2007GL030409\" target=\"_blank\" rel=\"noopener\">cross-gradient<\/a> and <a href=\"https:\/\/doi.org\/10.1016\/j.tecto.2004.10.010\" target=\"_blank\" rel=\"noopener\">multi-layer<\/a> joint inversion of potential field data.<\/li>\n\n\n\n<li class=\"has-palette-color-4-color has-text-color has-link-color has-medium-font-size wp-elements-79988f57f21209f64cff2d106bd7e1fa\">Identification of basins and possible cap layers.<\/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-6ec4d75\" data-v=\"4\" data-block-id=\"6ec4d75\"><style>.stk-6ec4d75 {align-self:center !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-6ec4d75-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-6ec4d75-inner-blocks\">\n<div class=\"wp-block-stackable-image stk-block-image stk-block stk-c2947f2\" data-block-id=\"c2947f2\"><figure><span class=\"stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4128\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/3D_joint_inversion_geothermal.jpg\" width=\"509\" height=\"332\"\/><\/span><\/figure><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div>\n\n<div class=\"wp-block-stackable-separator alignfull stk-block-separator stk--no-padding stk-block stk-54b8596 stk-block-background stk--has-background-overlay\" data-block-id=\"54b8596\"><style>.stk-54b8596 {background-image:url(https:\/\/ggi-geophysics.com\/wp-content\/uploads\/colorful-namafjal-llandscape-in-iceland-in-summer-2023-11-27-04-55-46-utc-scaled.jpg) !important;background-attachment:fixed !important;}.stk-54b8596:before{background-color:#000000 !important;opacity:0.4 !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>Geothermal Energy In a society with increasing energy consumption, geothermal energy plays a fundamental role among renewable alternatives, harnessing the Earth&#8217;s internal heat to generate continuous electrical energy. Geophysical methodologies are one of the best tools for identifying and assessing the availability of these geothermal resources in great detail. At GGI, we develop and apply [&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-4523","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\/4523","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=4523"}],"version-history":[{"count":5,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages\/4523\/revisions"}],"predecessor-version":[{"id":4526,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages\/4523\/revisions\/4526"}],"wp:attachment":[{"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/media?parent=4523"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}