{"id":4542,"date":"2024-05-07T08:46:26","date_gmt":"2024-05-07T06:46:26","guid":{"rendered":"https:\/\/ggi-geophysics.com\/hydrocarbons\/"},"modified":"2025-08-05T07:38:38","modified_gmt":"2025-08-05T05:38:38","slug":"hydrocarbons","status":"publish","type":"page","link":"https:\/\/ggi-geophysics.com\/en\/hydrocarbons\/","title":{"rendered":"Hydrocarbons"},"content":{"rendered":"\n<div class=\"wp-block-stackable-columns alignfull stk-block-columns stk-block stk-1c5eb6f\" data-block-id=\"1c5eb6f\"><style>.stk-1c5eb6f {margin-bottom:0px !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-1c5eb6f-column alignfull\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-2bed2d7 stk-block-background stk--has-background-overlay\" data-v=\"4\" data-block-id=\"2bed2d7\"><style>.stk-2bed2d7 {background-image:url(https:\/\/ggi-geophysics.com\/wp-content\/uploads\/2024\/05\/oil-platform-on-the-ocean-offshore-drilling-for-g-2023-11-27-05-28-34-utc-scaled.jpg) !important;}.stk-2bed2d7-container{min-height:268px !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-2bed2d7-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-2bed2d7-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-0975d8e\" id=\"hidrocarburos\" data-block-id=\"0975d8e\"><style>.stk-0975d8e {margin-top:82px !important;margin-left:43px !important;}@media screen and (max-width:689px){.stk-0975d8e {margin-top:22px !important;margin-right:-13px !important;margin-left:8px !important;}}<\/style><h1 class=\"stk-block-heading__text\">Hydrocarbons<\/h1><\/div>\n<\/div><\/div><\/div>\n<\/div><\/div>\n\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 {background-color:#1f1f44 !important;min-height:460px !important;align-items:center !important;margin-bottom:76px !important;display:flex !important;}.stk-c2a98d6:before{background-color:#1f1f44 !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-c2a98d6-column alignwide\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-d2199c0\" data-v=\"4\" data-block-id=\"d2199c0\"><style>.stk-d2199c0 {align-items:flex-end !important;display:flex !important;}<\/style><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-d2199c0-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-d2199c0-inner-blocks\">\n<p class=\"has-palette-color-5-color has-text-color has-link-color has-medium-font-size wp-elements-fdf5eddd01e96af10b69e5ece286edd4\">Nowadays, the identification and exploitation of hydrocarbon reservoirs poses ever-increasing challenges. These include the search for hidden reservoirs beneath saline horizons or extensive basaltic flows, as well as the application of improved stimulation methods for the recovery of residual hydrocarbons in reservoirs.  <\/p>\n\n\n\n<p class=\"has-palette-color-5-color has-text-color has-link-color has-medium-font-size wp-elements-d4d30d0235e290fe8ed6175aa65b9c13\">Current strategies for interpreting seismic sections and cubes seek not only to detect structures in greater detail but also to discern the characteristics of both the porous matrix and the different fluids contained within it. To address these new challenges, it is necessary to integrate different types of geophysical information that complement the images obtained from reflection seismic data, such as geophysical logs, electromagnetic data, and even gravity and magnetic data. This information is then applied using modern <a href=\"http:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2010RG000330\" target=\"_blank\" rel=\"noopener\">joint inversion<\/a> techniques.  <\/p>\n\n\n\n<p class=\"has-palette-color-5-color has-text-color has-link-color has-medium-font-size wp-elements-9613e6573cc72c3414c530a23c4f05c4\">At GGI <a href=\"https:\/\/ggi-geophysics.com\/servicios\/\" data-type=\"page\" data-id=\"39\">we have the capabilities<\/a> to assimilate various types of geophysical data and adjust them to structures identified by seismic sections and cubes. We also seek to increase depth resolution by using well information, jointly inverting cross-hole tomography (seismic or electromagnetic) data and geophysical logs. <\/p>\n<\/div><\/div><\/div>\n<\/div><\/div>\n\n<div class=\"wp-block-stackable-columns alignwide stk-block-columns stk-block stk-dc44dd2 stk-block-background\" data-block-id=\"dc44dd2\"><style>.stk-dc44dd2 {background-color:#1f1f44 !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;}.stk-dc44dd2:before{background-color:#1f1f44 !important;}<\/style><div class=\"stk-row stk-inner-blocks stk-block-content stk-content-align stk-dc44dd2-column alignwide\">\n<div class=\"wp-block-stackable-column stk-block-column stk-column stk-block stk-d984413\" data-v=\"4\" data-block-id=\"d984413\"><div class=\"stk-column-wrapper stk-block-column__content stk-container stk-d984413-container stk--no-background stk--no-padding\"><div class=\"stk-block-content stk-inner-blocks stk-d984413-inner-blocks\">\n<div class=\"wp-block-stackable-heading stk-block-heading stk-block-heading--v2 stk-block stk-1d7c0a7\" id=\"soluciones\" data-block-id=\"1d7c0a7\"><style>.stk-1d7c0a7 {margin-bottom:1px !important;}.stk-1d7c0a7 .stk-block-heading__text{color:var(--theme-palette-color-5, #E7EBEE) !important;}<\/style><h2 class=\"stk-block-heading__text has-text-color has-text-align-center\">Solutions<\/h2><\/div>\n\n\n\n<div class=\"wp-block-stackable-card alignfull stk-block-card stk-block stk-da17f23 is-style-horizontal\" data-v=\"2\" data-block-id=\"da17f23\"><style>.stk-da17f23 {margin-top:89px !important;margin-bottom:25px !important;}.stk-da17f23 .stk-block-card__content{min-height:195px !important;padding-left:48px !important;}.stk-da17f23 .stk-block-card__image{width:883px !important;height:100% !important;}@media screen and (max-width:999px){.stk-da17f23 .stk-block-card__image{width:300px !important;}}@media screen and (max-width:689px){.stk-da17f23 .stk-block-card__image{width:0px !important;}}<\/style><div class=\"stk--no-padding stk-container stk-da17f23-container stk--no-background stk--no-padding\"><figure class=\"stk-block-card__image stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4137\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/joint_cross-well_tomography.jpeg\" width=\"1458\" height=\"415\" srcset=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/joint_cross-well_tomography.jpeg 1458w, https:\/\/ggi-geophysics.com\/wp-content\/uploads\/joint_cross-well_tomography-768x219.jpeg 768w\" sizes=\"auto, (max-width: 1458px) 100vw, 1458px\" \/><\/figure><div class=\"stk-block-card__content\"><div class=\"stk-block-content stk-inner-blocks stk-da17f23-inner-blocks\">\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-0b7ecdf\" data-block-id=\"0b7ecdf\"><p class=\"stk-block-text__text has-text-align-center\"><span style=\"color: #ffffff;\" class=\"stk-highlight\">Geospectral section combining electrical resistivity (well log) and cross-ho<\/span><span style=\"color: #fefefe;\" class=\"stk-highlight\">le seismic velocity.<\/span><\/p><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-2976ada\" data-block-id=\"2976ada\"><style>.stk-2976ada {max-width:839px !important;min-width:auto !important;margin-right:auto !important;margin-left:auto !important;}<\/style><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-03937e6\" data-block-id=\"03937e6\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-03937e6\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-03937-e-6-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-03937-e-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-1fc6c53\" id=\"tomografia-cross-hole-de-datos-electromagneticos-y-sismicos-guiados-por-registros-de-pozo\" data-block-id=\"1fc6c53\"><style>.stk-1fc6c53 .stk-block-heading__text{color:var(--theme-palette-color-5, #E7EBEE) !important;}<\/style><h3 class=\"stk-block-heading__text has-text-color\">Cross-hole tomography of electromagnetic and seismic data guided by well logs<\/h3><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-4274461\" data-block-id=\"4274461\"><style>.stk-4274461 {max-width:839px !important;min-width:auto !important;margin-right:auto !important;margin-left:auto !important;}<\/style><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-e339bdf\" data-block-id=\"e339bdf\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-e339bdf\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-e-339-bdf-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-e-339-bdf-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-aaa0912\" id=\"inversion-2-d-y-3-d-de-datos-geofisicos-guiados-por-registros-de-pozo\" data-block-id=\"aaa0912\"><style>.stk-aaa0912 .stk-block-heading__text{color:var(--theme-palette-color-5, #E7EBEE) !important;}<\/style><h3 class=\"stk-block-heading__text has-text-color\">2D and 3D inversion of geophysical data guided by well logs<\/h3><\/div>\n<\/div><\/div>\n<\/div><\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-card stk-block-card stk-block stk-e9f556f is-style-horizontal\" data-v=\"2\" data-block-id=\"e9f556f\"><style>.stk-e9f556f {margin-top:107px !important;}.stk-e9f556f .stk-block-card__content{padding-left:48px !important;}.stk-e9f556f .stk-block-card__image{width:871px !important;height:100% !important;}@media screen and (max-width:999px){.stk-e9f556f .stk-block-card__image{width:300px !important;}}@media screen and (max-width:689px){.stk-e9f556f .stk-block-card__image{width:0px !important;}}<\/style><div class=\"stk--no-padding stk-container stk-e9f556f-container stk--no-background stk--no-padding\"><figure class=\"stk-block-card__image stk-img-wrapper stk-image--shape-stretch\"><img loading=\"lazy\" decoding=\"async\" class=\"stk-img wp-image-4139\" src=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/seismic_constrained_inversion.jpg\" width=\"1266\" height=\"667\" alt=\"Hydrocarbons\" srcset=\"https:\/\/ggi-geophysics.com\/wp-content\/uploads\/seismic_constrained_inversion.jpg 1266w, https:\/\/ggi-geophysics.com\/wp-content\/uploads\/seismic_constrained_inversion-768x405.jpg 768w\" sizes=\"auto, (max-width: 1266px) 100vw, 1266px\" \/><\/figure><div class=\"stk-block-card__content\"><div class=\"stk-block-content stk-inner-blocks stk-e9f556f-inner-blocks\">\n<div class=\"wp-block-stackable-text stk-block-text stk-block stk-687dde1\" data-block-id=\"687dde1\"><p class=\"stk-block-text__text has-text-align-center\"><span style=\"color: #ffffff;\" class=\"stk-highlight\">Geospectral image of density and magnetization guided by a seismic section.<\/span><\/p><\/div>\n\n\n\n<div class=\"wp-block-stackable-icon-label stk-block-icon-label stk-block stk-46601ec\" data-block-id=\"46601ec\"><style>.stk-46601ec {max-width:839px !important;min-width:auto !important;margin-right:auto !important;margin-left:auto !important;}<\/style><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-518a0df\" data-block-id=\"518a0df\"><span class=\"stk--svg-wrapper\"><div class=\"stk--inner-svg\"><svg style=\"height:0;width:0\"><defs><lineargradient id=\"linear-gradient-518a0df\" x1=\"0\" x2=\"100%\" y1=\"0\" y2=\"0\"><stop offset=\"0%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-518-a-0-df-color-1)\"><\/stop><stop offset=\"100%\" style=\"stop-opacity:1;stop-color:var(--linear-gradient-518-a-0-df-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-ec419e1\" id=\"a-href-http-library-seg-org-doi-10-1190-geo-2011-0394-1-inversion-de-datos-electromagneticos-y-potenciales-sujetos-a-volumenes-y-secciones-sismicas-en-hidrocarburos-a\" data-block-id=\"ec419e1\"><style>.stk-ec419e1 .stk-block-heading__text{color:var(--theme-palette-color-5, #E7EBEE) !important;}<\/style><h3 class=\"stk-block-heading__text has-text-color\"><a href=\"http:\/\/library.seg.org\/doi\/10.1190\/geo2011-0394.1\" target=\"_blank\" rel=\"noopener\">Inversion of electromagnetic and potential field data subject to seismic volumes and sections in hydrocarbons<\/a><\/h3><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-stackable-spacer stk-block-spacer stk--no-padding stk-block stk-c3cf9c9\" data-block-id=\"c3cf9c9\"><style>.stk-c3cf9c9 {height:157px !important;}<\/style><\/div>\n<\/div><\/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-12b776b stk-block-background stk--has-background-overlay\" data-block-id=\"12b776b\"><style>.stk-12b776b {background-image:url(https:\/\/ggi-geophysics.com\/wp-content\/uploads\/2025\/05\/oil-and-gas-refinery-plant-form-industry-zone-aer-2025-01-09-00-25-24-utc-scaled.jpg) !important;background-attachment:fixed !important;}.stk-12b776b: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\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Hydrocarbons Nowadays, the identification and exploitation of hydrocarbon reservoirs poses ever-increasing challenges. These include the search for hidden reservoirs beneath saline horizons or extensive basaltic flows, as well as the application of improved stimulation methods for the recovery of residual hydrocarbons in reservoirs. Current strategies for interpreting seismic sections and cubes seek not only to [&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-4542","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\/4542","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=4542"}],"version-history":[{"count":8,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages\/4542\/revisions"}],"predecessor-version":[{"id":4548,"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/pages\/4542\/revisions\/4548"}],"wp:attachment":[{"href":"https:\/\/ggi-geophysics.com\/en\/wp-json\/wp\/v2\/media?parent=4542"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}