Jun 28, 2023 · The common-depth-point (CDP) seismic-reflection method was used to delineate subsurface structure in a 3-m thick, 220-m deep coal zone in the Palau area of Coahuila, Mexico. An extensive series of walkaway- noise tests was performed to optimize recording pa- rameters and equipment. Reflection events can beIn this paper a method for depth migration of individual shot records followed by common depth point (CDP) stacking is described and iIIustrated with a real data example. First we explain the philosophy behind shot record migration. Then we go through the different stages of the procedure using a real data example.Common depth point (COP) recording, sometimes called common mid point (CMP), is a basic method in present day seismic exploration, whether that is the normal linear 2-D type or 3-D recording. However, to understand the concept fully, it is necessary to look back on the history of seismic exploration with respect, in the main, to the geometry of ...common depth point. 1. n. [Geophysics] In multichannel seismic acquisition where beds do not dip, the common reflection point at depth on a reflector, or the halfway point when a wave travels from a source to a reflector to a receiver. In the case of flat layers, the common depth …Nov 5, 2021 · The performance of two popular migration methods—the Kirchhoff integral and reverse‐time migrations—is evaluated through applications to imaging complex structures using prestack shot records. The migration results from the Marmousi model data demonstrate that reverse‐time migration is more accurate than Kirchhoff migration in …The results of a seismic reflection profiling exercise are strongly dependent upon parameters used in field recording. The choice of parameters is determined by objectives of the survey, available resources, and geologic locality. Some simple modeling and/or a walkaway noise survey are helpful in choice of field parameters. Filtering data before analog‐to‐digital …Nov 2, 2022 · Nonlinear 3D tomographic least-squares inversion of residual moveout in Kirchhoff prestack-depth-migration common-image gathers. Frank Adler, Reda Baina ... Nichols, and Sylvestre Charles, (1998), "Automated 3D tomographic velocity analysis of residual moveout in prestack depth migrated common image point gathers," SEG …Aug 24, 2018 · We look at an approach used to collect common midpoint data. Common midpoint acquisition provides a redundancy of observations from a local region (the Fresn... Fig. 1. Common events on a walkaway noise test reco rd. microcomputer for data acquisition and processing. High-resolution shallow reflection seismics can now be successfully applied to geological, engineering and environmental problems (e.g. Meekes et al. 1990, Pullan & Hunter 1990, Miller & Steeples 1994). The most commonly applied shallow reflection …DOI: 10.3997/1365-2397.1989017 Corpus ID: 130242784; Prestack migration by shot record inversion and common depth point stacking: a case study @article{Schoot1989PrestackMB, title={Prestack migration by shot record inversion and common depth point stacking: a case study}, author={A. Van Der Schoot and R. Romijn and David E. Larson and A. J. …Local prestack estimates of reflector orientations, which are computed for each CDP from 64 adjacent common depth point gathers, indicate a range of strike azimuths for the mantle reflector of 090 ... Jumpstart your career! Learn from a vast source of knowledge, that you know you need, but couldn’t find anywhere. Dive deep into lighting, CG techniques, materials, color, design and archviz business. And look at it all from a wider perspective. Whether you want to understand a subject in depth or need a good portion of inspiration. The sum of the traces of seismic reflection data, acquired from a roll-along survey, which correspond to the same common depth point but which originate from different seismic profiles and different offsets. The technique reduces substantially the amplitude of incoherent noise, multiples with their different normal moveouts, diffractions, etc ... The purpose of this work is to characterize the fluid accumulation zone in the first 150 m depth in the middle of the crater, using several post-stack seismic attributes and Amplitude Versus Offset ... This is the main reason behind the good quality of the obtained Common-Depth-Point ...The best method is to get an average bed slope of the reach BELOW your study reach and use that. Absent of that information, the two downstream points would ...With the constant flow of information in today’s digital age, staying up-to-date with the latest breaking news around the world is more important than ever. Breaking news has a sig...Dictionary. : Common-depth point (CDP) { {#category_index:C|common-depth point (CDP)}} The reflecting point that is common to a subset of data. The use of this term …The common depth point stack. Abstract: The Common Depth Point (CDP) Method is a seismic data acquisition and processing technique which transforms field recordings …The depth of the Columbia River ranges from 20 feet to 170 feet at various points along its route, and its total length is 1,243 miles. Locks, dams and reservoirs built on the Colu...The common depth point (CDP) was applied to get the subsurface reflectors. The CDP method included time corrections of wavelet arrivals (based on absolute offset and velocity) ...The most common standard is IEEE 754, which is composed of three fields: ... 32-bit floating point bit depth and 64-bit summing Reason 7 DAW by Propellerhead Software: 16-, 20- and 24-bit I/O, 32-bit floating point arithmetic …Lume Deodorant has been making waves in the beauty industry with its claims of being an effective and long-lasting solution for body odor. Lume Deodorant is a natural deodorant tha...For example, common conversion point (CCP) stacking is applied routinely in receiver functions studies (e.g. Dueker & Sheehan 1997; Gilbert et al. ... The traveltime difference Δt between transmitted P and converted S is a measure of interface depth, which is ambiguous at complex regions shown as question marks.Mar 28, 2000 · Common-midpoint gather. Common-midpoint gathers CMP (also called common-depth point CDP) are required for velocity analyses, Normal Moveout Correction NMO and for stacking. The whole line can be sorted so that it is in order of increasing CDP points and also so that the traces are in the order of increasing offset for each CDP point. process assigns each trace to a single shot, receiver, common depth point, inline, crossline, and offset bin. Other individual values for each trace, shot, receiver, CDP, and offset bin are also computed. The first step in the Geometry Assignment process, the description of the field geometry, can actually be accomplished using a number of ... The common-depth-point information is gathered for a plurality of incidence angles, (theta), of less than 20-30° such that assumptions concerning various elastic parameters, density, compressional-wave-velocity and shear-wave-velocity can be made which allow the application of linear fitting techniques to the gathered data. Common-conversion-point binning. We learned in analysis of amplitude variation with offset that an incident P -wave is partitioned at a layer boundary into reflected and transmitted P - and S -wave components. Consider the raypath geometry in Figure 11.6-30a for an incident P -wave generated by the source S1 and a flat reflector.Common Depth Point (CDP) Stacking . Seismic lines follow the available access routes and hence frequently are by no means as straight as desirable. The processing is therefore based on a line of section that smooths out the variations in the line. This CDP line is a curve of best fit through the midpoints between sources and receivers, which ...A pre-processed super common mid-point gather clearly shows the reflector event corresponding to the DMR1 at 17.25 s ... common depth-point (CDP) as well as common receiver domains.common midpoint. 1. n. [Geophysics] In multichannel seismic acquisition, the point on the surface halfway between the source and receiver that is shared by numerous source-receiver …We exploit estimates of P‐wave reflectivity from autocorrelation of transmitted teleseismic P arrivals and their coda in a common reflection point (CRP) migration technique. The approach employs the same portion of the vertical‐component seismogram, as in standard Ps receiver function analysis. This CRP prestack depth migration …Common-Mid-Point (CMP) Gathers. Common MASW surveys use a 1D linear receiver array (RA) to generate a 2D shear-wave velocity (Vs) cross section through a roll-along approach. Although surface waves spread into all azimuths, only the propagation along the path of the RA is used for subsequent analysis that generates a 1D velocity (Vs) profile to ...Common-offset depth migrations and traveltime tomography. January 1999. SEG Technical Program Expanded Abstracts. 10.1190/1.1888776. Authors: William Harlan. Retired.Nov 2, 2022 · The well‐known instability of Kunetz’s (1963) inversion algorithm can be explained by the progressive manner in which the calculations are done (descending from the surface) and by the fact that completely different impedances can yield indistinguishable synthetic seismograms. Those difficulties can be overcome by using an iterative …The Common Depth Point (CDP) Method is a seismic data acquisition and processing technique which transforms field recordings from seismic surveys into pseudo-cross-sectional images of …This research discuss the impact of studying the common depth point (CDP) gathers on Near, Mid and Far-offsets, to verify the credibility of the amplitude response in the prospect evaluation, through analyzing a case study of two exploratory wells; one has already penetrated a gas-bearing sandstone as a reservoir and the other one is dry-sand ...DOI: 10.3997/1365-2397.1989017 Corpus ID: 130242784; Prestack migration by shot record inversion and common depth point stacking: a case study @article{Schoot1989PrestackMB, title={Prestack migration by shot record inversion and common depth point stacking: a case study}, author={A. Van Der Schoot and R. Romijn and David E. Larson and A. J. …Feb 20, 2023 · Seismic imaging using conventional technologies was poor, and the subsurface structures and strata were unreliable for interpretation. We have applied an integrated processing-and-interpretation method based on seismic wavefield characteristics of common-scatterpoint (CSP) gathers to deal with the exploration challenges.Seismic Reflection Principles: Basics. Niranjan C. Nanda. Chapter. First Online: 11 March 2016. 3066 Accesses. 2 Citations. Abstract. Seismic reflection events are caused by …About common image point tomography. CIP-tomo is a generalized reflection tomography method that uses residual moveout (RMO, residual curvature) analysis of prestack depth-migrated CIP gathers to update an initial model. Multiparameter (nonhyperbolic, general, or nonparametric) RMO is automatically estimated from offset vector tile or angle ... 1. n. [Geophysics] In multichannel seismic acquisition where beds do not dip, the common reflection point at depth on a reflector, or the halfway point when a wave travels from a source to a reflector to a receiver. In the case of flat layers, the common depth point is vertically below the common midpoint. In the case of dipping beds, there is ... Mar 16, 2017 ... And a good starting point on bottom depth is a 1/8" pedestal. Many other things will change the sound. So just experiment. I made alot of ...Apr 11, 2019 · Untuk mendapatkan informasi lebih lanjut dan merinci mengenai istilah/kata common depth point, disarankan untuk merujuk pada sumber-sumber terpercaya seperti Kamus Besar Bahasa Indonesia (KBBI) yang dikeluarkan oleh Kementerian ...Common depth point (COP) recording, sometimes called common mid point (CMP), is a basic method in present day seismic exploration, whether that is the normal linear 2-D type or 3-D recording. However, to understand the concept fully, it is necessary to look back on the history of seismic exploration with respect, in the main, to the geometry of ...In order to overcome the noise problem and additionally to estimate earth velocity, the method of acquisition most commonly used is the Common-Mid-Point (CMP) method. The same method is also called Common-Depth-Point …2 Citations. Abstract. Of all the geophysical exploration methods, seismic surveying is unequivocally the most important, primarily because it is capable of detecting large-scale to …The Common Depth Point (CDP) Method is a seismic data acquisition and processing technique which transforms field recordings from seismic surveys into pseudo-cross-sectional images of the earth's geologic layering beneath the survey line. Such images are the primary geophysical analysis tools used by explorationists to pinpoint likely drilling …Aug 17, 2006 · In this paper, we tested both RTM and IM with seminatural Green's functions on a synthetic and a field common-depth-point (CDP) data set, the latter from the Gulf of Mexico (GOM). Results show that both RTM and IM can remove the significant kinematic distortions caused by the overburden without knowledge of the overburden velocity.• CDP bases input traces on their common depth point number. Used primarily for CDP gathers. • SOURCE, SOU_XD, or SOU_YD bases input records on the sequential source number or changes in coordinates within the file. To be used primarily for shot gathers. • REC_XD, or REC_YD bases input ensembles on changes in their receiver coordinates.Periodontitis, the most common oral disease, is a chronic inflammatory condition occur in response to bacterial plaque biofilms, characterized by the destruction of soft and …In snowy conditions, adequate tread depth is even more important. Tread depth by the numbers. A few key numbers to keep in mind when checking tread depth are: 10/32nds of an inch: the most common tread depth of a new tire. 6/32nds of an inch: the lowest tread depth still considered “good” by most tire experts.Nov 2, 2022 · The results of a seismic reflection profiling exercise are strongly dependent upon parameters used in field recording. The choice of parameters is determined by objectives of the survey, available resources, and geologic locality. Some simple modeling and/or a walkaway noise survey are helpful in choice of field parameters. Filtering data …Jul 30, 2023 · The two-dimensional (2-D) geophysical data in the BOEM inventory is common depth point (CDP) seismic information collected along a survey line. Also known as common midpoint or common reflection point data, the data are derived from a common location in the oceanNov 2, 2022 · The results of a seismic reflection profiling exercise are strongly dependent upon parameters used in field recording. The choice of parameters is determined by objectives of the survey, available resources, and geologic locality. Some simple modeling and/or a walkaway noise survey are helpful in choice of field parameters. Filtering data … Defining an adequate common depth-point (CDP) binning size is one of the first processing steps of any 3D seismic dataset. In fact, bins are carefully selected even during the planning and acquisition steps so that targets are properly imaged with high fold and resolution, also considering a uniform offset and azimuthal coverage for each CDP ... Blue Letter Bible is an invaluable online resource for those looking to delve into the depths of biblical study. Blue Letter Bible’s interface may seem overwhelming at first glance...The common-depth-point gather is conducted at angles of offset of less than 20-30 degrees such that assumptions concerning various elastic parameters: density, compressional wave velocity and shear-wave-velocity can be made which allow the application of linear fitting techniques to the gathered data. The sum of these coefficients …Field X area. Using Geomage software. Velocity analysis was carried out on three CDPs (Common Depth Point), CDP 480, CDP 826 and CDP 1740 to investigate good semblance pattern. Good semblance pattern is defined as a pattern which indicates regularity semblance of coherence maximum value, so it will be easy to pick the velocity values.Three-dimensional prestack depth migration and depth residual picking in common-image gathers (CIGs) are the most time-consuming parts of 3D migration velocity analysis. Most migration-based velocity analysis algorithms need spatial coordinates of reflection points and CIG depth residuals at different offsets (or angles) to provide …MULTICHANNEL COMMON DEPTH POINT (CDP) SEISMIC REFLECTION DATA ADDITIONAL ATLANTIC SURVEY LINES Data Announcement 1979N-N. The National Geophysical Data Center (now the National Centers for Environmental Information) is making available additional CDP seismic reflection data (lines 7, 8, 11, 12, and 13).Common depth method (CDM) improves the signal-to-noise ratio of a seismic shot. By repeating the shots and measuring them from slightly different positions ...For those who are looking for a more efficient and cost-effective way to dry their clothes, a 27 inch depth gas dryer is an excellent choice. This type of dryer is becoming increas... Common depth point (CDP) Common depth point (COP) recording, sometimes called common mid point (CMP), is a basic method in present day seismic exploration, whether that is the normal linear 2-D type or 3-D recording. However, to understand the concept fully, it is necessary to look back on the history With the constant flow of information in today’s digital age, staying up-to-date with the latest breaking news around the world is more important than ever. Breaking news has a sig...The common-depth-point gather is conducted at angles of offset of less than 20-30 degrees such that assumptions concerning various elastic parameters: density, compressional wave velocity and shear-wave-velocity can be made which allow the application of linear fitting techniques to the gathered data. The sum of these coefficients corresponds ...List of common depths. 1-bit color 2 colors, often black and white (or whatever color the CRT ... Linear color space and floating point. More bits also encouraged the storage of light as linear values, where the number directly corresponds to the amount of light emitted. Linear levels makes calculation of computer graphics much easier. Seismic surveying is the most important of the three main types of geophysical prospecting. To understand this method, a review of the physical principles that govern the movement of acoustic or shock waves through layered media is necessary. Consider a source of acoustic energy at a point on the Earth’s surface. Metode horizon based depth tomography untuk mengidentifikasi struktur pada lapangan “x” 2D pre stack depth migration (PSDM) common reflection angle migration (CRAM) menggunakan perangkat keras meliputi CPU (Central Processing Unit), computer 2 layar (30 inci) dengan system operasi linux (read head) milik perusahaan PT.Sep 15, 2020 · • Common depth point (CDP) adalah geometri raypath dimana sinyal hasil pantulan dari satu titik reflect shot direkam oleh sekelompok receiver yang berbeda. • Common source point (CSP) adalah geometri raypath …In snowy conditions, adequate tread depth is even more important. Tread depth by the numbers. A few key numbers to keep in mind when checking tread depth are: 10/32nds of an inch: the most common tread depth of a new tire. 6/32nds of an inch: the lowest tread depth still considered “good” by most tire experts.A steeply dipping crustal fault that extends from the surface near CDP (Common Depth Point) 150 to its truncation by the E reflectors at ~30 km depth near CDP 400 has been interpreted from the ... 1. Common-Depth Point Seismic Data: 24-Fold multichannel seismic data for 5 lines, 26 sections (full scale) available in plastic sepia, paper sepia, and blackline. 2. Other Geophysical Data: 3. Merged navigation, magnetics and bathymetric data are available in MGD77 format on 1 magnetic tape or CD-ROM. Feb 21, 2022 ... Based on residual move-out analysis of re- flectors in common image point gathers, an update of the velocity is estimated by a ray-based ...MULTICHANNEL COMMON DEPTH POINT (CDP) SEISMIC REFLECTION DATA Additional Atlantic Survey Lines Data Announcement 1980SE-BB. The National Geophysical Data Center (now the National Centers for Environmental Information) is making available CDP seismic reflection data for lines 18 through 38 from Atlantic coastal areas.The most common standard is IEEE 754, which is composed of three fields: ... 32-bit floating point bit depth and 64-bit summing Reason 7 DAW by Propellerhead Software: 16-, 20- and 24-bit I/O, 32-bit floating point arithmetic …Insular shelves are underwater landmasses surrounding islands. They are relatively shallow areas that extend from the low waterline, usually to a depth of about 100 fathoms, where ...Abstract: The Common Depth Point (CDP) Method is a seismic data acquisition and processing technique which transforms field recordings from seismic surveys into pseudo-cross-sectional … The subject method includes the gathering of common-depth-point information for a plurality of incidence angles, (theta) and estimating the linear coefficients (R /SUB pp/ . /SUB o/ and R /SUB pp/ ./sub 1/)of a linear function fitted to the amplitudes vs. sin/sup 2/ (theta) measured for each point of reflection. This is called the Common Depth Point (CDP) method because the data is repeatedly recorded over increasing source to receiver offsets, but with the raypaths reflecting off the same depth location on each geological surface. The CDP gather shown in figure 7 (b) shows the recorded traces for all source / receiver pairs.Feb 12, 2024 · Cookies help us deliver our services. By using our services, you agree to our use of cookies. Approximately 2,500 km of underway geophysical data, including 430 km of 24-channel common depth point (CDP) seismic-reflection data for purchase from the National Geophysical Data Center (NGDC) (now the National Centers for Environmental Information (NCEI)). The data were collected in the eastern equatorial Pacific Ocean offshore Nicaragua and ... Jul 30, 2023 · The two-dimensional (2-D) geophysical data in the BOEM inventory is common depth point (CDP) seismic information collected along a survey line. Also known as common midpoint or common reflection point data, the data are derived from a common location in the ocean1. n. [Geophysics] In multichannel seismic acquisition where beds do not dip, the common reflection point at depth on a reflector, or the halfway point when a wave travels from a source to a reflector to a receiver.In the case of flat layers, the common depth point is vertically below the common midpoint.In the case of dipping beds, there is no common …Are you ready to embark on an exhilarating gaming adventure? Look no further than Slope Game Online. This fast-paced and addictive game has taken the online gaming community by sto...The Common Depth Point (CDP) Method is a seismic data acquisition and processing technique which transforms field recordings from seismic surveys into pseudo-cross-sectional images of the earth's geologic layering beneath the survey line. Such images are the primary geophysical analysis tools used by explorationists to pinpoint likely drilling …The normal at any given subsurface location to the propagating wave front points in the direction of what we commonly think of as a ray. Since the propagation ...When it comes to choosing a new iPhone, one of the most important factors to consider is the size. With different iPhone models offering varying sizes, it’s essential to find the p...1. Common-Depth Point Seismic Data: 12- and 24-fold multichannel seismic data for 27 sections (full scale) available in plastic sepia, paper sepia and blackline. 2. Other Geophysical Data: 3.5 kHz and 12 kHz profiler records and magnetic profiles on 1 roll of 35-mm microfilm (No. 2098) 3. Merged digital navigation, magnetics and bathymetric ...Oct 7, 2014 · Common-conversion-point binning. We learned in analysis of amplitude variation with offset that an incident P -wave is partitioned at a layer boundary into reflected and transmitted P - and S -wave components. Consider the raypath geometry in Figure 11.6-30a for an incident P -wave generated by the source S1 and a flat reflector. The common depth point method (CDP) with 12 fold coverage was adopted for the survey.Several artefacts were noticed on the result of the seismic migrated section, when the fk filter was initially ...Illustration of common depth point (often called common mid point). Arrivals on a seismic reflection record can be seen in figure 4. The receivers are arranged to one side of a shot, …
Seismic Reflection Principles: Basics. Niranjan C. Nanda. Chapter. First Online: 11 March 2016. 3066 Accesses. 2 Citations. Abstract. Seismic reflection events are caused by …. Ultra surf
Figure 23 Common midpoint gather. During the stacking phase of processing the data is resorted into common midpoint gathers using the survey geometry information. This is also referred to as the Common Depth Point or CDP. The number of source receiver pairs that produce reflections at the same point is referred to as the fold. The fold and ...1. Common-Depth Point Seismic Data: 12- and 24-fold multichannel seismic data for 27 sections (full scale) available in plastic sepia, paper sepia and blackline. 2. Other Geophysical Data: 3.5 kHz and 12 kHz profiler records and magnetic profiles on 1 roll of 35-mm microfilm (No. 2098) 3. Merged digital navigation, magnetics and bathymetric ...Data Announcement 87-MGG-03. Approximately 2,233-km of 24-channel common depth point (CDP) seismic-reflection profiles for purchase from the National Geophysical Data Center (NGDC) (now the National Centers for Environmental Information (NCEI)) for the Pacific Outer Continental Shelf off northern California and Oregon.The Common Depth Point (CDP) Method is a seismic data acquisition and processing technique which transforms field recordings from seismic surveys into pseudo-cross-sectional images of …The treads on your tires keep you safe on the road, but only if they aren’t worn. Learn more about what constitutes a tire’s good depth, what tread depth of a new tire should be, t...FIG. 3. Schematic diagram for 3-D depth-variant common conversion point (CCP) Binning For a single, horizontal, homogeneous layer, as shown in Figure 2, according to Snell's law, we can derive the following relation y2(X_-2+1)- (2hT2Xc'2)2 t-1, (4) where Zc is the depth of the conversion point, Xc is the horizontal distance between theCommon depth method (CDM) improves the signal-to-noise ratio of a seismic shot. By repeating the shots and measuring them from slightly different positions ...Dec 14, 2021 ... Common depth cues the brain uses to perceive depth without stereo vision. And for bonus points, notice that the "cylinders" aren't actually ...We exploit estimates of P‐wave reflectivity from autocorrelation of transmitted teleseismic P arrivals and their coda in a common reflection point (CRP) migration technique. The approach employs the same portion of the vertical‐component seismogram, as in standard Ps receiver function analysis. This CRP prestack depth migration …In recent years, electric scooters have gained immense popularity as a more sustainable and efficient mode of transportation. One such scooter that has caught the attention of many...The common depth point (CDP) was applied to get the subsurface reflectors. The CDP method included time corrections of wavelet arrivals (based on absolute offset and velocity) ...Variasi desain akuisisi seismik 2D yang dianalisa pada penelitian ini adalah Common depth point Interval (CDP Interval), Fold Coverage, dan Far Offset. Target formasi yang dianalisa adalah Formasi Jatibarang bagian atas dengan kedalaman 1763 meter dan terletak pada domain waktu seismik 1000 ms.MULTICHANNEL COMMON DEPTH POINT (CDP)SEISMIC REFLECTION DATA. Data Announcement 1976-R. * Third Data Set: Seismic data for Three Additional Atlantic Survey lines. As part of a program by the U.S. Geological Survey (USGS) to gain a better understanding of the general geologic framework of the Continental Shelf, Slope, and …The point is entered only in those images that see a tie point location best. Depth tie point require depth maps in the \TEMP directory of the mission. See Compute depth maps for more information. To enter a new depth point: 1. Select Add depth command from the Point pulldown menu. The Add common depth point dialog opens: 2.The common-depth-point information is gathered for a plurality of incidence angles, (theta), of less than 20-30° such that assumptions concerning various elastic parameters, density, compressional-wave-velocity and shear-wave-velocity can be made which allow the application of linear fitting techniques to the gathered data.Feb 21, 2022 ... Based on residual move-out analysis of re- flectors in common image point gathers, an update of the velocity is estimated by a ray-based ...The standard practice in DUG's service division is to use a velocity sampled at around 100m x 100m x 24ms/20m unless there is a strong reason for more density.However, it may also be partly due to differences in the sensitivity of PP versus PS images to illumination angles and/or differences in the spatial locations of subsurface sampling (common-depth points versus common-conversion points) due to 3D geometry. 5) The dips observed on the PS images are generally flatter than on the PP images.Illustration of common depth point (often called common mid point). Arrivals on a seismic reflection record can be seen in figure 4. The receivers are arranged to one side of a shot, ….