{"id":247,"date":"2012-03-28T17:43:43","date_gmt":"2012-03-28T13:43:43","guid":{"rendered":"https:\/\/www.zond-geo.co\/english\/?page_id=247"},"modified":"2017-12-10T19:01:11","modified_gmt":"2017-12-10T15:01:11","slug":"zondmag3d","status":"publish","type":"page","link":"https:\/\/www.zond-geo.co\/english\/zond-software\/gravity-magnetic-self-potential\/zondmag3d\/","title":{"rendered":"ZondGM3D"},"content":{"rendered":"ZondGM3d<\/strong>\u00a0program is designed \u00a0for three-dimensional interpretation of gravity \u00a0and magnetic data by (land and aero variants).\r\n\r\nAnomalies of gravity caused of different dense heterogeneity are investigated in gravity survey. Influence of host rocks \u00a0and surrounding topography is excluded by subtraction of \u00a0the normal field and reductions.\r\n\r\nMagnetic survey is studied field generated by rocks that contain ferromagnetic minerals. Connection of measured on the surface field with magnetic properties of rocks allows to conclude about existence of \u00a0magnetic objects.\r\n

ZondGM3d<\/strong><\/strong><\/strong>\u00a0represents ready solution for gravity and magnetic methods, and solves wide range of problems from mathematical modeling \u00a0to field data processing and interpretation. Convenient interface and variety of data visualization features allow to solve wide range of geological problems with maximum effectiveness.<\/p>\r\n

ZondGM3d<\/strong><\/strong><\/strong>\u00a0uses simple and clear data format which allows easily combining various systems of observation, including different variants of the topography setting up and other additional information.<\/p>\r\nSpecial graphics mode \u00a0that allows to visualize data in the freandly form is presented.\r\n

Some variants of three-dimensional model display in the form of various sections and isosurfaces are realized in the program.<\/p>\r\n

Important stage which prevents field measurement is mathematical modeling of petrophysical structure of work site. Modeling gives a chance \u00a0to make a choice of optimum parameters of the observation system for decision of formulated geological problem.<\/p>\r\n

\"3D<\/a><\/p>\r\n

As the general task of the program is inversion of density and magnetic susceptibility, some variants of inverse problem decision are realized in\u00a0ZondGM3d<\/strong>, basic of them are: smoothing inversion \u2013 to get smooth model and focusing \u2014 to get \u00a0piece-smoothed model of petrophysical parameters with depth.<\/p>\r\nWhile program was designed special consideration given to a priori data accounting. Because of equivalence of inverse geophysical problems, quality of the obtained results strongly depends on the amount of a priori data\u00a0used. In\u00a0ZondGM3d<\/strong>\u00a0there is possibility of weights setting for measurements, fixing and limits making of changing features of different cells, using of a priori model as reference \u00a0in inversion. There is also possibility to import and display results of measurements by other methods and cross-boreholes data that improved quality of results.\r\n

\"3D<\/a><\/p>\r\n \r\n

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Version 13 \/ 12 \/ 2023\u00a0|\u00a0 Software: download<\/a>|Video lesson: download<\/a><\/p>\r\n\r\n<\/div>\r\n<\/div>","protected":false},"excerpt":{"rendered":"

ZondGM3d\u00a0program is designed \u00a0for three-dimensional interpretation of gravity \u00a0and magnetic data by (land and aero variants). Anomalies of gravity caused of different dense heterogeneity are investigated in gravity survey. Influence of host rocks \u00a0and surrounding topography is excluded by subtraction of \u00a0the normal field and reductions. Magnetic survey is studied field generated by rocks that […]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":36,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":"","_links_to":"","_links_to_target":""},"class_list":["post-247","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/247","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/comments?post=247"}],"version-history":[{"count":15,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/247\/revisions"}],"predecessor-version":[{"id":1411,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/247\/revisions\/1411"}],"up":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/36"}],"wp:attachment":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/media?parent=247"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}