{"id":239,"date":"2012-03-28T17:40:08","date_gmt":"2012-03-28T13:40:08","guid":{"rendered":"https:\/\/www.zond-geo.co\/english\/?page_id=239"},"modified":"2018-10-28T20:56:33","modified_gmt":"2018-10-28T16:56:33","slug":"zondst2d","status":"publish","type":"page","link":"https:\/\/www.zond-geo.co\/english\/zond-software\/seismic-tomography\/zondst2d\/","title":{"rendered":"ZondST2D"},"content":{"rendered":"<strong>ZondST2d<\/strong> is designed \u00a0for two-dimensional interpretation of <strong>seismic tomography<\/strong>\u00a0data on refracted and reflected waves (land, cross-borehole and water variants).\r\n\r\nThe software includes the following modules: 1. <a href=\"https:\/\/www.youtube.com\/watch?v=P9LS6h7nHS0\">MASW\/ReMi<\/a> &#8211; surface waves data processing and interpretation, 2. Refraction waves forward modeling and inversion in arbitrary layered medium , 3. <a href=\"https:\/\/www.youtube.com\/watch?v=lGc6I8W8Kck\">attenuation tomography<\/a>, 4. velocity anisotropy, 5. <a href=\"https:\/\/www.youtube.com\/watch?v=IU728b0GpD0&amp;feature=youtu.be\">Reflection waves forward modeling and inversion<\/a> in arbitrary layered medium.\r\n<p style=\"text-align: justify;\">In geophysics,\u00a0the term\u00a0<strong>seismic tomography<\/strong>\u00a0is known\u00a0for a long time.\u00a0This is due to\u00a0the fact that one\u00a0of the main problems in\u00a0seismology\u00a0&#8211;\u00a0the inverse\u00a0kinematics.\u00a0It consists in determining the\u00a0velocity structure at\u00a0a known\u00a0time\u00a0path of the refracted waves\u00a0from \u00a0source to receiver. \u00a0The most popular\u00a0in engineering\u00a0geophysics\u00a0was\u00a0crosshole Seismotomography.\u00a0This direction is used\u00a0for detailed\u00a0studies of \u00a0rocks\u00a0velocity structure \u00a0in the interborehole space.<\/p>\r\n<strong>ZondST2d<\/strong> represents ready solution for <strong>seismic tomography<\/strong>, and solves wide range of problems from mathematical modeling and quality control to field data processing and interpretation. Convenient interface and variety of data visualization features allow to solve wide range of geological problems with maximum effectiveness.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_1.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-258\" style=\"width: 540px; height: 327px;\" title=\"First arrivals times picking in ZondST2D. Refraction tomography.\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_1.png\" alt=\"First arrivals times picking in ZondST2D. Refraction tomography.\" width=\"1230\" height=\"861\" \/><\/a><\/p>\r\nThe software consists of two basic modules. One for the first times picking on the seismograms. The second is used for solving forward and inverse problems of seismic tomography.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_2.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-258\" style=\"width: 540px; height: 327px;\" title=\"MASW processing in ZondST2d\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_2.png\" alt=\"MASW processing in ZondST2d\" width=\"1206\" height=\"749\" \/><\/a><\/p>\r\nFor the seismograms processing developed a special interface designed to simplify and automate the process of <a href=\"https:\/\/www.youtube.com\/watch?v=zgJgf8RvRI8\">first arrivals times picking<\/a>. Special attention is paid to variety ways of data visualization and simple access to frequently used functions.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_3.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-258\" style=\"width: 540px; height: 327px;\" title=\"MASW profile inversion in ZondST2d\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_3.png\" alt=\"MASW profile inversion in ZondST2d\" width=\"1206\" height=\"749\" \/><\/a><\/p>\r\nSolution of forward problem basis on special ray tracing algorithm of graph theory (Shortest path&#8217;s method). This algorithm is characterized by a high-speed calculations, and controlled accuracy.\r\n\r\n<strong>ZondST2d<\/strong> uses 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.\r\n\r\nImportant stage which prevents field measurement is <a href=\"https:\/\/www.youtube.com\/watch?v=KQf83dh60Ek\">mathematical modeling of velocity structure<\/a> for <strong>seismic tomography<\/strong> survey. Modeling gives a chance to estimate the level of reflected waves first times and to make a choice of optimum parameters of the observation system for decision of formulated geological problem. <strong>ZondSt2d<\/strong> has great range of tools for mathematical modeling and analysis of refracted and reflected waves.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_4.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-258\" style=\"width: 540px; height: 327px;\" title=\"Layered inversion for refracted seismic data in ZondST2d\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_4.png\" alt=\"Layered inversion for refracted seismic data in ZondST2d\" width=\"1145\" height=\"832\" \/><\/a><\/p>\r\nAs the general task of the program is inversion of velocity parameters, some variants of <strong>seismic tomography<\/strong> inverse problem solutions are designed\u00a0in <strong>ZondST2d<\/strong>, basic of them are: smoothing inversion \u2013 to get smooth model and focusing &#8211; to get \u00a0piece-smoothed model of velocities with depth.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_5.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-258\" style=\"width: 540px; height: 327px;\" title=\"Attenuation tomography and inversion for anisotropy of velocities\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_5.png\" alt=\"Attenuation tomography and inversion for anisotropy of velocities\" width=\"1147\" height=\"831\" \/><\/a><\/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 <strong>ZondST2d<\/strong> there 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. The robust schemas of noise estimation\u00a0are designed\u00a0in the software. There is also possibility to import and display results of measurements by other methods and boreholes data that improved quality of results.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_6.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-258\" style=\"width: 540px; height: 327px;\" title=\"Velocity inversion results and geological interpretation of section.\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondST2d_6.png\" alt=\"Velocity inversion results and geological interpretation of section.\" width=\"930\" height=\"794\" \/><\/a><\/p>\r\nBasic features:\r\n<ul>\r\n\t<li>Measurements at the water surface and the water bottom. Borehole and cross-borehole systems. Any mixed system.<\/li>\r\n\t<li>Four ways for specifying topography. Real-time editing.<\/li>\r\n\t<li>Buffer for 5 models.<\/li>\r\n\t<li>A set of tools for mathematical modeling of velocity section. <a href=\"https:\/\/www.youtube.com\/watch?v=yen12nbSzPw\">Standard mesh \u201cbitmap\u201d style, arbitrary layered model and polygonal style model<\/a>. Additional tools for gravity, magnetic forward modeling and for joint inversion(Vp&amp;VS, MASW, reflection and refraction, TDEM, VES, gravity and magnetic).<\/li>\r\n\t<li>Number of the inversion algorithms : smooth, focusing, robust, block. Setting the reference model for the inversion. Suppression of the noise component during inversion (robust reweighting).<\/li>\r\n\t<li>Suppressing static shifts during inversion.<\/li>\r\n\t<li>Setting of limits for models parameters, inserting of a priori geological boundaries and borehole data to inversion. Assignment of weights for datum records. Editor of measurements.<\/li>\r\n\t<li>Estimation of results quality based on sensitivity matrix analysis. Calculation of sensitivity, quality and DOI index.<\/li>\r\n\t<li>Number of variants for data, model and apriori information visualization. Ability to set a semitransparent background for the resistivity section (geological, seismic sections).<\/li>\r\n\t<li>Three-dimensional visualization of the velocity sections along arbitrary system profiles. Maps slices of parameters for various depths.<\/li>\r\n\t<li>Geological sections editor and borehole columns editor. Titled boreholes.<\/li>\r\n\t<li>Exporting to bitmap and vector graphics formats, excel, surfer, AUTOCAD. Setting the scale of the exported image. Print images and create reports.<\/li>\r\n<\/ul>\r\nExtra app for <a href=\"https:\/\/www.zond-geo.co\/zfiles\/nakamura.zip\">Nakamura method<\/a>. \u00a0(<a href=\"https:\/\/www.youtube.com\/watch?v=8U14zz8FCNE\">Video<\/a>)\r\n<div class=\"finfo\">\r\n<div class=\"finfo-in\">\r\n<p align=\"center\">Version 13 \/ 12 \/ 2023\u00a0|\u00a0 Software: <a href=\"https:\/\/www.zond-geo.co\/zfiles\/ZondST2D.zip\">download<\/a> \u00a0|\u00a0 Video lesson: <a href=\"https:\/\/www.youtube.com\/watch?v=w0OLFBzZU1c\">download<\/a><\/p>\r\n\r\n<\/div>\r\n<\/div>","protected":false},"excerpt":{"rendered":"<p>ZondST2d is designed \u00a0for two-dimensional interpretation of seismic tomography\u00a0data on refracted and reflected waves (land, cross-borehole and water variants). The software includes the following modules: 1. MASW\/ReMi &#8211; surface waves data processing and interpretation, 2. Refraction waves forward modeling and inversion in arbitrary layered medium , 3. attenuation tomography, 4. velocity anisotropy, 5. Reflection waves [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":34,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":"","_links_to":"","_links_to_target":""},"class_list":["post-239","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/239","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=239"}],"version-history":[{"count":29,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/239\/revisions"}],"predecessor-version":[{"id":2041,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/239\/revisions\/2041"}],"up":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/34"}],"wp:attachment":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/media?parent=239"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}