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(PDF) Optimizing 3D Seismic Data Analysis Methods

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Consequently, the available technologies, the costs involved in acquiring new data and the possibilities for using existing data needed to be evaluated when planning the project.","publication_date":"2007,,","publication_name":"In Mapping Doggerland: the Mesolithic Landscapes of the Southern North Sea, Archaeopress, Editors: Gaffney, V, Thomson, K. \u0026 Fitch, S ","grobid_abstract_attachment_id":"37109944"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"3D Seismic Reflection Data, Associated Technologies and the Development of the Project Methodology.","broadcastable":true,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [114659]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "full_page_mobile_sutd_modal"; window.loswp.useOptimizedScribd4genScript = false; window.loginModal = {}; window.loginModal.appleClientId = 'edu.academia.applesignon'; window.userInChina = "false";</script><script defer="" src="https://accounts.google.com/gsi/client"></script><div class="ds-loswp-container"><div class="ds-work-card--grid-container"><div class="ds-work-card--container js-loswp-work-card"><div class="ds-work-card--cover"><div class="ds-work-cover--wrapper"><div class="ds-work-cover--container"><button class="ds-work-cover--clickable js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;swp-splash-paper-cover&quot;,&quot;attachmentId&quot;:37109944,&quot;attachmentType&quot;:&quot;pdf&quot;}"><img alt="First page of “3D Seismic Reflection Data, Associated Technologies and the Development of the Project Methodology.”" class="ds-work-cover--cover-thumbnail" src="https://0.academia-photos.com/attachment_thumbnails/37109944/mini_magick20190304-1279-xr5elo.png?1551769817" /><img alt="PDF Icon" class="ds-work-cover--file-icon" src="//a.academia-assets.com/images/single_work_splash/adobe_icon.svg" /><div class="ds-work-cover--hover-container"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span><p>Download Free PDF</p></div><div class="ds-work-cover--ribbon-container">Download Free PDF</div><div class="ds-work-cover--ribbon-triangle"></div></button></div></div></div><div class="ds-work-card--work-information"><h1 class="ds-work-card--work-title">3D Seismic Reflection Data, Associated Technologies and the Development of the Project Methodology.</h1><div class="ds-work-card--work-authors ds-work-card--detail"><a class="ds-work-card--author js-wsj-grid-card-author ds2-5-body-md ds2-5-body-link" data-author-id="114659" href="https://bradford.academia.edu/VincentGaffney"><img alt="Profile image of Vincent Gaffney" class="ds-work-card--author-avatar" src="https://0.academia-photos.com/114659/30829/28347/s65_vincent.gaffney.jpg" />Vincent Gaffney</a></div><div class="ds-work-card--detail"><p class="ds-work-card--detail ds2-5-body-sm">2007, In Mapping Doggerland: the Mesolithic Landscapes of the Southern North Sea, Archaeopress, Editors: Gaffney, V, Thomson, K. &amp; Fitch, S </p><div class="ds-work-card--work-metadata"><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">visibility</span><p class="ds2-5-body-sm" id="work-metadata-view-count">…</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">description</span><p class="ds2-5-body-sm">10 pages</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">link</span><p class="ds2-5-body-sm">1 file</p></div></div><script>(async () => { const workId = 11650016; const worksViewsPath = "/v0/works/views?subdomain_param=api&amp;work_ids%5B%5D=11650016"; const getWorkViews = async (workId) => { const response = await fetch(worksViewsPath); if (!response.ok) { throw new Error('Failed to load work views'); } const data = await response.json(); return data.views[workId]; }; // Get the view count for the work - we send this immediately rather than waiting for // the DOM to load, so it can be available as soon as possible (but without holding up // the backend or other resource requests, because it's a bit expensive and not critical). const viewCount = await getWorkViews(workId); 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} })();</script></div><p class="ds-work-card--work-abstract ds-work-card--detail ds2-5-body-md">A variety of methods and datasets were potentially available for use in the project. However, as the choice of methods, and hence data types, controls the volume and quality of the results an optimal approach needed to be developed. A crucial consideration was the need to minimise the time involved in the analysis, and hence the expense of the project, whilst at the same time maximising the spatial coverage and detail. Consequently, the available technologies, the costs involved in acquiring new data and the possibilities for using existing data needed to be evaluated when planning the project.</p><div class="ds-work-card--button-container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;continue-reading-button--work-card&quot;,&quot;attachmentId&quot;:37109944,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;workUrl&quot;:&quot;https://www.academia.edu/11650016/3D_Seismic_Reflection_Data_Associated_Technologies_and_the_Development_of_the_Project_Methodology&quot;}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;download-pdf-button--work-card&quot;,&quot;attachmentId&quot;:37109944,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;workUrl&quot;:&quot;https://www.academia.edu/11650016/3D_Seismic_Reflection_Data_Associated_Technologies_and_the_Development_of_the_Project_Methodology&quot;}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div><div class="ds-signup-banner-trigger-container"><div class="ds-signup-banner-trigger ds-signup-banner-trigger-control"></div></div><div class="ds-signup-banner ds-signup-banner-control"><div id="ds-signup-banner-close-button"><button class="ds2-5-button ds2-5-button--secondary ds2-5-button--inverse"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">close</span></button></div><div class="ds-signup-banner-ctas"><img src="//a.academia-assets.com/images/academia-logo-capital-white.svg" /><h4 class="ds2-5-heading-serif-sm">Sign up for access to the world's latest research</h4><button class="ds2-5-button ds2-5-button--inverse ds2-5-button--full-width js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;signup-banner&quot;}">Sign up for free<span class="material-symbols-outlined" style="font-size: 20px" translate="no">arrow_forward</span></button></div><div class="ds-signup-banner-divider"></div><div class="ds-signup-banner-reasons"><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Get notified about relevant papers</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Save papers to use in your research</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Join the discussion with peers</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Track your impact</span></div></div></div><script>(() => { // Set up signup banner show/hide behavior: // 1. 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In practice, fine-scale and regular acquisition geometry is possible only in 2-D seismic surveys. 3-D surveys typically have sparse and irregular geometry that often results in spatial aliasing. In this paper we present a processing method to overcome this problem that is suitable for sparse and irregular acquisition geometry, and yields better results than does conventional processing such as dip moveout.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Spatial dealiasing of 3-D seismic reflection data&quot;,&quot;attachmentId&quot;:42748805,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/16100566/Spatial_dealiasing_of_3_D_seismic_reflection_data&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/16100566/Spatial_dealiasing_of_3_D_seismic_reflection_data"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="1" data-entity-id="106377610" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/106377610/A_Comparative_Case_Study_of_Reflection_Seismic_Imaging_Method">A Comparative Case Study of Reflection Seismic Imaging Method</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="213352" href="https://olemiss.academia.edu/AdnanAydin">Adnan Aydin</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Geological Society of America Abstracts with Programs, 2017</p><p class="ds-related-work--abstract ds2-5-body-sm">Reflection seismology is the most common and effective method to gather information on the earth interior. The quality of seismic images is highly variable depending on the complexity of the underground and on how seismic data are acquired and processed. One of the crucial steps in this process, especially in layered sequences with complicated structure, is the time and/or depth migration of seismic data. The primary purpose of the migration is to increase the spatial resolution of seismic images by repositioning the recorded seismic signal back to its original point of reflection in time/space, which enhances information about the complex structure. In this study, our objective is to process a seismic dataset (courtesy of the University of South Carolina) to generate an image on which the Magruder fault near Allendale SC can be distinguished, and its attitude can be accurately depicted. The data was gathered by common mid-point method with 60 geophones equally spaced along an about 550 m long traverse over a nearly flat ground. In the future, we will apply different migration algorithms (including finite-difference and Kirchhoff), and the results will be compared in time and depth domains to investigate the efficiency of each algorithm in reducing the processing time and improving the accuracy of seismic images in reflecting the correct position of the Magruder fault. iii DEDICATION I would have liked to dedicate this thesis to my lovely parents and kind brother for all their endless support, love, and encouragements throughout my life but since the earthquake occurred in Kermanshah, province in the western part of Iran, on 12 November 2017 at 18:18 UTC, which it caused the most significant damage and loss of life, while I was writing my thesis in Oxford, Mississippi, far from the motherland, this thesis is dedicated to the kind, patient and brave people of Kermanshah. May the improvement in seismic knowledge and techniques provide the safer and happier life for all people around the world, especially for all kids.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;A Comparative Case Study of Reflection Seismic Imaging Method&quot;,&quot;attachmentId&quot;:105591819,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/106377610/A_Comparative_Case_Study_of_Reflection_Seismic_Imaging_Method&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/106377610/A_Comparative_Case_Study_of_Reflection_Seismic_Imaging_Method"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="2" data-entity-id="96554736" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/96554736/Some_problems_with_seismic_reflection_techniques">Some problems with seismic reflection techniques</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="176068048" href="https://independent.academia.edu/GregoryBlackburn">Gregory Blackburn</a></div><p class="ds-related-work--metadata ds2-5-body-xs">1982</p><p class="ds-related-work--abstract ds2-5-body-sm">Idealised view of a reflection profile. 2.2 Schematic geological section depicting areas for velocity analysis. 2.6 2.3 Schematic geological section showing actual raypaths and hypothetical raypaths for a vertical CRP. 2.10 2.4 Schematic geological section containing a high velocity inhomogeneity. 2.10 2.5 Schematic T 2-X2 plots for a reflector whose arrival time due to migration or raypath distortion problems is earlier than for the homogeneous case (A) or where the arrival time is later than expected (B). 2.11</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Some problems with seismic reflection techniques&quot;,&quot;attachmentId&quot;:98421138,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/96554736/Some_problems_with_seismic_reflection_techniques&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/96554736/Some_problems_with_seismic_reflection_techniques"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="3" data-entity-id="13870966" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/13870966/SeisPrho_An_interactive_computer_program_for_processing_and_interpretation_of_high_resolution_seismic_reflection_profiles">SeisPrho: An interactive computer program for processing and interpretation of high-resolution seismic reflection profiles</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="32954420" href="https://independent.academia.edu/GiuseppeStanghellini">Giuseppe Stanghellini</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="33084294" href="https://unibo.academia.edu/LucaGasperini">Luca Gasperini</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Computers &amp; Geosciences, 2009</p><p class="ds-related-work--abstract ds2-5-body-sm">SEISPRHO is an interactive computer program for processing and interpreting high-resolution seismic reflection profiles developed using the Delphi/Kylix multiplatform programming environment. For this reason, it is available under Windows TM and Linux TM operating systems. The program allows the users to handle SEG-Y data files (and other non-standard formats) carrying out a processing sequence over the data to obtain, as a final result, bitmap images of seismic sections. Some basic algorithms are implemented, including filtering and deconvolution. However, the main feature of SEISPRHO is its interactive graphic interface, which provides the user with several tools for interpreting the data, such as reflector picking and map digitizing. Moreover, the program allows importing and geo-referencing maps and seismic profiles in the form of digital images. Trace-by-trace analysis of seismic signal and sea-bottom reflectivity is also implemented, as well as other special functions such as compilation of time-slice maps from close-spaced grids of seismic lines. SEISPRHO is distributed as public domain software for non-commercial purposes by the Marine Geology division of the Istituto di Scienze Marine (ISMAR-CNR). This paper is an introduction to the program and a preliminary guide to the users.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;SeisPrho: An interactive computer program for processing and interpretation of high-resolution seismic reflection profiles&quot;,&quot;attachmentId&quot;:44856787,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/13870966/SeisPrho_An_interactive_computer_program_for_processing_and_interpretation_of_high_resolution_seismic_reflection_profiles&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/13870966/SeisPrho_An_interactive_computer_program_for_processing_and_interpretation_of_high_resolution_seismic_reflection_profiles"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="4" data-entity-id="34949587" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/34949587/SEISMIC_REFLECTION_METHODS_APPLIED_TO_ENGINEERING_ENVIRONMENTAL_AND_GROUND_WATER_PROBLEMS">SEISMIC REFLECTION METHODS APPLIED TO ENGINEERING, ENVIRONMENTAL, AND GROUND-WATER PROBLEMS</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="70419773" href="https://independent.academia.edu/EdwinYefersonRamosCanaza">Edwin Yeferson Ramos Canaza</a></div><p class="ds-related-work--abstract ds2-5-body-sm">The seismic-reflection method is a powerful geophysical exploration method that has been in widespread use in the petroleum industry for more than 60 years. Since 1980, it has been increasingly used in applications shallower than 30 m, and that is the principal subject of this paper. The seismic-reflection method measures different parameters than other geophysical methods, and it requires careful attention to avoid possible pitfalls in data collection, processing, and interpretation. Part of the key to avoiding the pitfalls is to understand the resolution limits of the technique, and to carefully plan shallow-reflection surveys around the geologic objective and the resolution limits. Careful planning is also necessary to make the method increasingly cost effective relative to test drilling and/or other geophysical methods. The selection of seismic recording equipment, energy source, and data-acquisition parameters are often critical to the success of a shallow-reflection project. It is important to carefully follow known seismic reflections throughout the data-processing phase to avoid misinterpretation of things that look like reflections but are not. The shallow-reflection technique has recently been used in mapping bedrock beneath alluvium in the vicinity of hazardous waste sites, detecting abandoned coal mines, following the top of the saturated zone during a pump test in an alluvial aquifer, and in mapping shallow faults. As resolution improves and cost-effectiveness increases, other new applications will be added.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;SEISMIC REFLECTION METHODS APPLIED TO ENGINEERING, ENVIRONMENTAL, AND GROUND-WATER PROBLEMS&quot;,&quot;attachmentId&quot;:54811844,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/34949587/SEISMIC_REFLECTION_METHODS_APPLIED_TO_ENGINEERING_ENVIRONMENTAL_AND_GROUND_WATER_PROBLEMS&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/34949587/SEISMIC_REFLECTION_METHODS_APPLIED_TO_ENGINEERING_ENVIRONMENTAL_AND_GROUND_WATER_PROBLEMS"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="5" data-entity-id="22894760" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/22894760/CHAPTER_II_BASIC_THEORY_2_1_Basic_Concept_of_Seismic_Reflection">CHAPTER II BASIC THEORY 2.1 Basic Concept of Seismic Reflection</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="44575941" href="https://independent.academia.edu/BimoGunners">Bimo Gunners</a></div><p class="ds-related-work--abstract ds2-5-body-sm">The seismic reflection method which has been used for underground exploration for over 60 years (Dobrin, 1976; Coffeen, 1978; Waters, 1997) is being used in the 1980s for targets shallower than 30m. Advances in microelectronics have resulted in construction of engineering seismographs and microcomputers that permit cost effective collection and processing of seismic reflection data in numerous applications Unique features of the seismic reflection method applicable to shallow engineering, groundwater, and environmental projects are described and recent applications are illustrated. A nonmathematical discussion of seismic methods and the differences between reflection, refraction, and borehole seismology are given. The seismic reflection method is compared with ground-penetrating radar. A set of high quality shallow seismic reflection data *introduces the fundamentals of seismic reflection and a seismic data processing discussion. Pitfalls of data processing and interpretation are introduced, including spatial aliasing, recognition of refractions in reflection data, and problems with air-coupled waves. Because successful use of the shallow seismic reflection method requires proper field data acquisition techniques, a discussion of geologic targets, site logistics, and parameter selection for various situations is included. Differences in the criteria for selection of seismic sources, seismographs, and geophones for shallow surveys as opposed to deeper surveys are given. Because the shallow seismic reflection method has not been widely used in production, a short discussion of field data collection efficiency and costs which could be of use to contractors in the initial stages of planning a geotechnical site investigation is provided. Case histories show file utility of the shallow seismic reflection Method in detecting faults, cavities and intra-alluvial stratigraphy. Use of the method in characterizing geologic, hydrologic, and stratigraphic conditions within 3m to 30m of the earth&#39;s surface is increasing. Seismic reflection techniques depend on the presence of acoustical contrasts in the subsurface. In many cases the acoustical contrasts occur at boundaries between geologic layers, although man-made boundaries such as tunnels and mines also represent contrasts. Acoustical contrasts occur as variations in either mass density or seismic velocity or both. The measure of acoustical contrast is formally known as acoustic impedance, which is simply the product of mass density and the speed of seismic waves traveling within a material. Figure 2.1 The simplest case of seismic reflection. S represents the source and R represents the receiver. Layer I represents an acoustical discontinuity.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;CHAPTER II BASIC THEORY 2.1 Basic Concept of Seismic Reflection&quot;,&quot;attachmentId&quot;:43434158,&quot;attachmentType&quot;:&quot;docx&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/22894760/CHAPTER_II_BASIC_THEORY_2_1_Basic_Concept_of_Seismic_Reflection&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/22894760/CHAPTER_II_BASIC_THEORY_2_1_Basic_Concept_of_Seismic_Reflection"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="8300102" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/8300102/The_use_of_shallow_seismic_reflection_surveys_in_environmental_studies">The use of shallow seismic reflection surveys in environmental studies</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="16506135" href="https://unibuc.academia.edu/AMihai">Andrei Mihai</a></div><p class="ds-related-work--abstract ds2-5-body-sm">The environmental studies involve the knowledge of the geological structure in the investigated areas. Such information can be obtained using various types of observations, geological and geophysical. The seismic reflection survey is known as the type of geophysical investigation which provides us accurate information regarding the velocity distribution into the ground. In addition, the obtained time sections offer an image about the geological structure of the subsurface. In this paper, we present the results of the use of shallow seismic reflection surveys in a multi-disciplinary project in which one of the main goals was the obtaining of clear structural information for the first 50 m of the ground. Good results were obtained after the seismic data processing. Their interpretation provided structural images that could be correlated with those given by other types of geophysical surveys, for example electrical surveys.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;The use of shallow seismic reflection surveys in environmental studies&quot;,&quot;attachmentId&quot;:34710191,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/8300102/The_use_of_shallow_seismic_reflection_surveys_in_environmental_studies&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/8300102/The_use_of_shallow_seismic_reflection_surveys_in_environmental_studies"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="34568033" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/34568033/Processing_of_Seismic_Reflection_Data">Processing of Seismic Reflection Data</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="68264853" href="https://independent.academia.edu/PhamTuanAnh23">Pham Tuan Anh</a></div><p class="ds-related-work--abstract ds2-5-body-sm">In this chapter, the steps are discussed of how to obtain a seismic reflectivity image from seismic records. Here, we assume that the records only contain reflections. Before we discuss these steps, we derive which property gives a reflection back from a boundary: the impedance contrast, also called the reflectivity. Then we will discuss the main basic steps of a processing sequence, commonly used to obtain a seismic image and common to seismic data gathered on land (onshore) as well as at sea (offshore): CMP sorting, velocity analysis and NMO correction, stacking, (zero-offset) migration and time-to-depth conversion. 5.1 Making the seismic image: seismic velocity As said in the last chapter, the goal of exploration seismics is obtaining structural subsur-face information from seismic data. In the previous chapter we discussed different types of &quot; noise &quot; that are always present in raw seismic records. In this chapter we assume that we analyze and process data that contain only primary reflected waves, and therefore we assume that we have somehow removed all the noise elements. The task now is to obtain an image of the subsurface from these data. In this chapter, we will look at a basic processing sequence to obtain a seismic image from the raw seismic data, containing only reflections. The most important information that must be added to the data, is the seismic velocity. This is crucial for obtaining a proper image. In this chapter it is discussed how to obtain a first estimate of the seismic velocities of the subsurface, and how to use this information to make the final image. The problem can also be seen as being information we measure at the surface, which is a function of time, is mapped to the correct position in depth. In other words, we want to convert &quot; time &quot;-data to &quot; depth &quot;-data. 78</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Processing of Seismic Reflection Data&quot;,&quot;attachmentId&quot;:54433606,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/34568033/Processing_of_Seismic_Reflection_Data&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/34568033/Processing_of_Seismic_Reflection_Data"><span class="ds2-5-text-link__content">View PDF</span><span 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You can download the paper by clicking the button above.</p></div></div></div></div><div class="ds-sidebar--container js-work-sidebar"><div class="ds-related-content--container"><h2 class="ds-related-content--heading">Related papers</h2><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="0" data-entity-id="117059773" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/117059773/The_application_of_extensive_3D_Seismic_Reflection_Data_for_the_exploration_of_extensive_inundated_Palaeolandscapes">The application of extensive 3D Seismic Reflection Data for the exploration of extensive inundated Palaeolandscapes</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1003217" href="https://bradford.academia.edu/SimonFitch">Simon Fitch</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2013</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;The application of extensive 3D Seismic Reflection Data for the exploration of extensive inundated Palaeolandscapes&quot;,&quot;attachmentId&quot;:113019567,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/117059773/The_application_of_extensive_3D_Seismic_Reflection_Data_for_the_exploration_of_extensive_inundated_Palaeolandscapes&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-related-work-grid-card-view-pdf" href="https://www.academia.edu/117059773/The_application_of_extensive_3D_Seismic_Reflection_Data_for_the_exploration_of_extensive_inundated_Palaeolandscapes"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="1" data-entity-id="8575607" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/8575607/Planning_Land_3_D_Seismic_Surveys">Planning Land 3-D Seismic Surveys</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="17701774" href="https://independent.academia.edu/AndresAmbros">Andres Ambros</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline 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data-entity-id="65271314" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/65271314/Some_considerations_on_shallow_seismic_reflection_surveys">Some considerations on shallow seismic reflection surveys</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="32134152" href="https://independent.academia.edu/RobertoBalia">Roberto Balia</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of Applied Geophysics, 2000</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Some considerations on shallow seismic reflection 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Amin Baban</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Arabian Journal of Geosciences, 2013</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Study of subsurface structures using seismic reflection data for Kalar–Khanaqin area/Kurdistan region, Iraq&quot;,&quot;attachmentId&quot;:69478248,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/52020615/Study_of_subsurface_structures_using_seismic_reflection_data_for_Kalar_Khanaqin_area_Kurdistan_region_Iraq&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-related-work-grid-card-view-pdf" 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