Archive of Digital Boomer and Chirp Seismic Reflection Data Collected During USGS Cruise 04SCC01 in Terrebonne, Timbalier, and Barataria Bays and Lake Pelto, Louisiana, June and July 2004

Metadata also available as - [Outline] - [Parseable text] - [XML]

Frequently anticipated questions:

What does this data set describe?

Title:
Archive of Digital Boomer and Chirp Seismic Reflection Data Collected During USGS Cruise 04SCC01 in Terrebonne, Timbalier, and Barataria Bays and Lake Pelto, Louisiana, June and July 2004
Abstract:
In June and July of 2004, the U.S. Geological Survey, in cooperation with the University of New Orleans, conducted geophysical surveys in Terrebonne Bay, Timbalier Bay, Lake Pelto, and Barataria Bay, Louisiana, and nearby waterbodies. This report serves as an archive of unprocessed digital boomer and chirp seismic reflection data, trackline maps, navigation files, GIS information, Field Activity Collection System (FACS) logs, observer's logbook, and formal FGDC metadata. Filtered and gained digital images of the seismic profiles are also provided.
The archived trace data are in standard Society of Exploration Geophysicists (SEG) SEG-Y format (Barry and others, 1975) and may be downloaded and processed with commercial or public domain software such as Seismic Unix (SU). Example SU processing scripts and USGS software for viewing the SEG-Y files (Zihlman, 1992) are also provided.
For more information on the seismic surveys see http://walrus.wr.usgs.gov/infobank/g/g104la/html/g-1-04-la.meta.html
These data are also available via GeoMapApp (http://www.geomapapp.org/) and Virtual Ocean ( http://www.virtualocean.org/) earth science exploration and visualization applications.
Supplemental_Information:
The USGS Florida Integrated Science Center (FISC) - St. Petersburg assigns a unique identifier to each cruise or field activity. For example, 04SCC01 tells us the data were collected in 2004 for the Subsidence and Coastal Change (SCC) study and the data were collected during the first field activity for that study in that calendar year. Refer to http://walrus.wr.usgs.gov/infobank/programs/html/definition/activity.html for a detailed description of the method used to assign the cruise ID. The naming convention used for each seismic line is as follows: yye##a, where yy is the last two digits of the year in which the data were collected, e is a 1-letter abbreviation for the equipment type (for example, b for boomer and c for chirp), ## is a 2-digit number representing a specific track, and a is a letter representing the section of a line if recording was prematurely terminated or rerun for quality or acquisition problems. The boomer plate is an acoustic energy source that consists of capacitors charged to a high voltage and discharged through a transducer in the water. The transducer is towed on a sled at the sea surface and when discharged emits a short acoustic pulse, or shot, that propagates through the water and sediment column. The acoustic energy is reflected at density boundaries (such as the seafloor or sediment layers beneath the seafloor), detected by a receiver, and recorded by a PC-based seismic acquisition system. This process is repeated at timed intervals (for example, 0.25 s) and recorded for specific intervals of time (for example, 100 ms). In this way, a two-dimensional vertical image of the shallow geologic structure beneath the ship track is produced. A C-Products C-Boom power supply was used for lines 04b01-04b25, and an Applied Acoustic Engineering CSP 300 power supply was used for lines 04b26a-04b37. For all lines, an Applied Acoustics AA200 plate was used and the power supplies provided 100 J per shot. Reflected energy was received by a Benthos MESH streamer and recorded by Delph Seismic acquisition software. The streamer, which was positioned parallel to the boomer sled and laterally separated from it by about 7 m, contains 10 hydrophones evenly spaced about every 30.5 cm (every 12 inches). Refer to figure 1 included with this archive (Data Series 237) for a diagram of boomer acquisition geometry. Sample frequency of the data was 16-20 kHz, and record length was 99-100 ms. Based on survey speeds of 3.5-4 knots and a shot rate of every 0.25 s, shot spacing was about 0.5 m. The chirp system uses a signal of continuously varying frequency. The sound source and receiver is a towfish, which is typically flown 2-5 m above the seafloor. For each recorded shot of the chirp data, 3 channels of trace data are collected. Channel 3 is the "real," or in-phase component of the signal, channel 2 is the "imaginary," or quadrature component of the signal, and channel 1 is the "envelope," or product of channels 2 and 3. Only channel 1 was used to produce the profiles presented here. However, all channels are included in the SEG-Y data files. The seismic source employed for chirp data collection consisted of an EdgeTech SB-424 towfish running FSSB software. Refer to figure 2 included with this archive (Data Series 237) for a diagram of chirp acquisition geometry, which varied during this cruise. The frequency range was 4-24 kHz. Sample frequency of the data was 25 kHz, and record length was 42-49 ms. Based on survey speeds of 3.5-4 knots and a shot rate of 0.125-0.25 s, shot spacing was about 0.25-0.5 m. The unprocessed seismic data are stored in SEG-Y, integer, Motorola format, which is a standard digital format that can be read and manipulated by most seismic processing software packages (Barry and others, 1975). The SEG-Y formatted trace files have a .TRA extension. Additional recording parameters for each trace file can also be found in the .PAR file associated with each .TRA file. However, the .PAR and .PLN files included here are only needed to process or display the data with Delph Seismic software. The SEG-Y files will not fit on one disc. They are distributed onto three DVDs with all boomer lines (04b01-04b37) on disc 1, chirp lines 04c01-04c24b on disc 2, and chirp lines 04c25-04c37b on disc 3. Also provided are example Seismic Unix scripts that allow the user to strip off navigation fixes from the SEG-Y headers, along with a fix for every 500 shots (boomer) or every 1,000 shots (chirp), and produce a filtered and gained GIF image of each profile. The printable profiles provided here are GIF images that were filtered and gained using Seismic Unix software. The processed SEG-Y data were exported to Chesapeake Technology, Inc. (CTI) SonarWeb software to produce interactive versions of the profiles that allow the user to obtain a geographic location and depth from the profile for a curser position. This information is displayed in the status bar of the browser. Warning! The only supported web browsers that properly display all features of the interactive profiles are Internet Explorer 6 for Windows and Firefox 1.5 for all platforms. For all browsers, the status bar and JavaScript must be enabled. Firefox also requires "Change status bar text" to be checked under Advanced JavaScript Options. Caution use of other browsers may result in spurious or no information given in the status window. Firefox may be downloaded at http://www.mozilla.org/products/firefox.
  1. How might this data set be cited?
    Calderon, Karynna, Dadisman, Shawn V., Flocks, James G., Kulp, Mark A., Miner, Michael D., Wiese, Dana S., and Harrison, Arnell S., 2006, Archive of Digital Boomer and Chirp Seismic Reflection Data Collected During USGS Cruise 04SCC01 in Terrebonne, Timbalier, and Barataria Bays and Lake Pelto, Louisiana, June and July 2004: U.S. Geological Survey Data Series 237, U.S. Geological Survey, St. Petersburg, FL.

    Online Links:

  2. What geographic area does the data set cover?
    West_Bounding_Coordinate: -90.832399
    East_Bounding_Coordinate: -89.837681
    North_Bounding_Coordinate: 29.45217
    South_Bounding_Coordinate: 29.03641
  3. What does it look like?
    DVD/maps/cruisenav/boomer.jpg (JPEG)
    Location map of all digital boomer seismic reflection data collected during USGS Cruise 04SCC01. This map was created at a scale of 1:625,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp.jpg (JPEG)
    Location map of all digital chirp seismic reflection data collected during USGS Cruise 04SCC01. This map was created at a scale of 1:625,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_a.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area A (refer to Area A of the boomer location map) during USGS Cruise 04SCC01. This map was created at a scale of 1:300,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_a.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area A (refer to Area A of the chirp location map) during USGS Cruise 04SCC01. This map was created at a scale of 1:300,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_b.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area B (refer to Area B of the boomer location map) during USGS Cruise 04SCC01. This map was created at a scale of 1:300,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_b.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area B (refer to Area B of the chirp location map) during USGS Cruise 04SCC01. This map was created at a scale of 1:300,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_1.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area 1 (refer to Area 1 of the boomer Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_1.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area 1 (refer to Area 1 of the chirp Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_2.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area 2 (refer to Area 2 of the boomer Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_2.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area 2 (refer to Area 2 of the chirp Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_3.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area 3 (refer to Area 3 of the boomer Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_3.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area 3 (refer to Area 3 of the chirp Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_3a.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area 3a (refer to Area 3a of the boomer Area 3 map) during USGS Cruise 04SCC01. This map was created at a scale of 1:25,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_3a.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area 3a (refer to Area 3a of the chirp Area 3 map) during USGS Cruise 04SCC01. This map was created at a scale of 1:25,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_4.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area 4 (refer to Area 4 of the boomer Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_4.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area 4 (refer to Area 4 of the chirp Area A map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_5.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area 5 (refer to Area 5 of the boomer Area B map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_5.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area 5 (refer to Area 5 of the chirp Area B map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/boomer_6.jpg (JPEG)
    Trackline map of digital boomer seismic reflection data collected in Area 6 (refer to Area 6 of the boomer Area B map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
    DVD/maps/cruisenav/chirp_6.jpg (JPEG)
    Trackline map of digital chirp seismic reflection data collected in Area 6 (refer to Area 6 of the chirp Area B map) during USGS Cruise 04SCC01. This map was created at a scale of 1:100,000. Refer to the Lineage section below for the trackline map creation process.
  4. Does the data set describe conditions during a particular time period?
    Beginning_Date: 30-Jun-2004
    Ending_Date: 08-Jul-2004
    Currentness_Reference:
    Data collection interval
  5. What is the general form of this data set?
    Geospatial_Data_Presentation_Form: Seismic Reflection Profile Section
  6. How does the data set represent geographic features?
    1. How are geographic features stored in the data set?
      Indirect_Spatial_Reference:
      Horizontal X and Y locations (latitude and longitude and UTMs) for each shot are provided as ASCII text files, along with the date and time (UTC) the shot was recorded.
    2. What coordinate system is used to represent geographic features?
      Horizontal positions are specified in geographic coordinates, that is, latitude and longitude. Latitudes are given to the nearest 0.000009. Longitudes are given to the nearest 0.000009. Latitude and longitude values are specified in Decimal degrees. The horizontal datum used is WGS84.
      The ellipsoid used is WGS84.
      The semi-major axis of the ellipsoid used is 6378137.
      The flattening of the ellipsoid used is 1/298.257.
  7. How does the data set describe geographic features?
    Entity_and_Attribute_Overview:
    Binary data file: Trace data are available as binary files in SEG-Y format. These files have a .TRA extension and range in size from 4.2 to 156 MB.
    Entity_and_Attribute_Overview:
    Graphic image file: Printable profiles are available as GIF images. Interactive profiles are available as HTML pages with accompanying JPEG images. The line navigation maps and trackline maps are JPEG images. The trackline maps contain links to the seismic profiles and line navigation maps.
    Entity_and_Attribute_Overview:
    Navigation file: Navigation files are available as ASCII text files. Provided are raw (unedited) shotpoint navigation files, edited shotpoint navigation files, and edited 500- or 1,000-shot-interval location files.
    Entity_and_Attribute_Overview:
    GIS file: The GIS project used to create the trackline maps is provided as a zip file composed of ESRI map documents, shapefiles, and metadata.
    Entity_and_Attribute_Detail_Citation:
    Barry, K.M., Cavers, D.A., and Kneale, C.W., 1975, Recommended standards for digital tape formats: Geophysics, v. 40, no. 2, p. 344-352. Also available online at http://www.seg.org/publications/tech-stand.
    Entity_and_Attribute_Detail_Citation:
    Zihlman, F.N., 1992, DUMPSEGY V1.0: A program to examine the contents of SEG-Y disk-image seismic data: U.S. Geological Survey Open-File Report 92-590, 28 p. Also available online at http://pubs.er.usgs.gov/usgspubs/ofr/ofr92590.

Who produced the data set?

  1. Who are the originators of the data set? (may include formal authors, digital compilers, and editors)
    • Karynna Calderon
    • Shawn V. Dadisman
    • James G. Flocks
    • Mark A. Kulp
    • Michael D. Miner
    • Dana S. Wiese
    • Arnell S. Harrison
  2. Who also contributed to the data set?
    Funding and (or) support for this study were provided by the USGS Coastal and Marine Geology Program and the University of New Orleans. We thank R/V G.K. Gilbert captains Dave Bennett (Eckerd College) and Richard W. Young (USGS FISC - St. Petersburg) for their assistance in data collection. This document was improved by the reviews of Randy Edwards (University of South Florida) and Charlene Sullivan (ETI Professionals, Inc., contracted by the USGS FISC - St. Petersburg).
  3. To whom should users address questions about the data?
    J. Flocks
    U.S. Geological Survey
    Geologist
    600 4th Street South
    St. Petersburg, FL
    USA

    (727) 803-8747, ext. 3012 (voice)
    jflocks@usgs.gov

Why was the data set created?

The data archived here were collected in cooperation with the University of New Orleans as part of the USGS Subsidence and Coastal Change (SCC) study.

How was the data set created?

  1. From what previous works were the data drawn?
  2. How were the data generated, processed, and modified?
    Date: 2004 (process 1 of 6)
    Boomer and chirp processing: The original trace files for lines 04b02, 04b26, 04b30, 04b31, 04b35, 04c02, 04c04, 04c06, 04c08a, 04c09, 04c10, 04c12, 04c13, 04c15a, 04c17, 04c18, 04c22, 04c24, 04c26-04c31, and 04c33-04c37 were divided into two or more trace files each (for example, 04b02 became 04b02a and 04b02b) because the original total number of traces exceeded the maximum allowed by the processing software. Original lines 04c08 and 04c15 were not modified. When divided, original line 04c08a became 04c08a and 04c08b, and original line 04c15a became 04c15a and 04c15b. The SEG-Y data were processed with Seismic Unix to produce GIF images of the seismic profiles included in this report. A representative boomer processing sequence consisted of 1) bandpass filtering: 300-500-2500-3000 Hz, 2) applying automatic gain control, 3) displaying PostScript, and 4) converting of PostScript image to GIF image. A representative chirp data processing sequence consisted of 1) stripping off channel 1 for each shot and converting to SU format, 2) applying automatic gain control, 3) displaying Postscript, and 4) converting of PostScript image to a GIF image. The processed SEG-Y data were then exported to CTI SonarWeb software to produce an interactive version of each profile that allows the user to obtain a geographic location and depth from the profile for a cursor position. Refer to the Supplemental Information section above for details on how to use the interactive profiles.
    Date: 2004 (process 2 of 6)
    Navigation processing: Shotpoint navigation files and 500- or 1,000-shot-interval location files were extracted from the trace headers of each line using Seismic Unix software and edited to remove or correct spurious data points. These files were then processed with PROJ.4 software (http://www.remotesensing.org/proj) to generate latitude and longitude from UTMs and reformatted for use with Environmental Systems Research Institute (ESRI) GIS software.
    Date: 2004 (process 3 of 6)
    Trackline map creation: The trackline maps provided in this archive were created using ESRI ArcView 3.3 and ArcGIS 8.3 software, exported to Adobe Illustrator for further editing, and saved in JPEG format. The maps are unprojected (geographic coordinates, NAD83). The USGS is the originator of all layers used. A map of trackline navigation for each seismic profile was also produced with CTI SonarWeb software.
    Date: 2004 (process 4 of 6)
    Data Series preparation: In addition to the process steps described above, the following steps were taken to produce this Data Series: the handwritten logs were scanned and saved as PDF files, digital FACS logs were created using the handwritten logs and personal accounts of the crew members and saved as PDF files, and an HTML-based format was used to present the various parts of this archive.
    Date: 24-Jan-2017 (process 5 of 6)
    Keywords section of metadata optimized for discovery in USGS Coastal and Marine Geology Data Catalog. Person who carried out this activity:
    U.S. Geological Survey
    Attn: Alan O. Allwardt
    Contractor -- Information Specialist
    2885 Mission Street
    Santa Cruz, CA

    831-460-7551 (voice)
    831-427-4748 (FAX)
    aallwardt@usgs.gov
    Date: 13-Oct-2020 (process 6 of 6)
    Added keywords section with USGS persistent identifier as theme keyword. Person who carried out this activity:
    U.S. Geological Survey
    Attn: VeeAnn A. Cross
    Marine Geologist
    384 Woods Hole Road
    Woods Hole, MA

    508-548-8700 x2251 (voice)
    508-457-2310 (FAX)
    vatnipp@usgs.gov
  3. What similar or related data should the user be aware of?

How reliable are the data; what problems remain in the data set?

  1. How well have the observations been checked?
    The validity or accuracy of marine seismic reflection profiles is highly qualitative and depends on equipment and operating condition variables. Visual inspection of the images rendered from the data did not show any major anomalies. Although data were collected in UTM Zones 15 and 16, all equipment was set to Zone 15 for this cruise. An unknown equipment failure occurred during acquisition of line 04c25 at about shot 2,450. A bug in the acquisition software resulted in no decimal values for UTMs being recorded in the SEG-Y headers for most of the boomer lines. The coastline layer used to create the trackline maps includes swamps and shallow, sandy areas exposed at low tide. For this reason, tracklines sometimes appear to traverse land.
  2. How accurate are the geographic locations?
    As the seismic reflection data were acquired, the position of the vessel was continuously determined by a CSI Wireless DGPS Max receiver, which is accurate within 3-5 m. Positions were recorded and written to the trace headers in Zone 15 UTMs about every 1 s. The ASCII navigation files and trackline maps have not been corrected to reflect the approximately 20-m offset between the boomer midpoint and GPS antenna or the varying (approximately 2-6 m) offset between the chirp and GPS antenna. Refer to figures 1 and 2 included with this archive (Data Series 237) for diagrams of acquisition geometry, including the GPS offset measurements. Line navigation maps and interactive profiles generated with CTI SonarWeb software have been corrected for the GPS offset.
  3. How accurate are the heights or depths?
    These data are not to be used for bathymetry. Boomer data are relative to sea level. However, varying recorded static shifts of the data have been known to occur. Depths shown on the chirp profiles are relative to the depth of the towfish, not to sea level. Furthermore, the raising or lowering of the towfish during a survey (to avoid obstacles or follow relief) produces a relative shift in the multiple reflections seen in the profile, which may be confused as a geologic feature. Any elevation change of the towfish is recorded in the logbooks and is evident on the seismic profiles by steep, abrupt shifts in the seafloor return.
  4. Where are the gaps in the data? What is missing?
    These data are collected along tracklines (2-D) and are therefore inherently incomplete. Geologic details between lines must be inferred. No data were collected for line 04b09. Only the upper 30 ms of a total 42-49 ms are displayed on the chirp profiles because little useful information was observed deeper in the sections. Navigation fixes are missing for the first 5,310 shots of line 04c17a, the first 230 shots of line 04c32, and the first 460 shots of line 04c37a. On the trackline maps, a cross marks the location of the first available navigation fix for these lines. Navigation fixes are also intermittent for several lines. On the trackline maps, missing navigation data within a line is inferred by linear interpolation of the first and last known data points. A yellow line indicates a navigation gap of 2 minutes or more.
  5. How consistent are the relationships among the observations, including topology?
    This data set is from one cruise with consistent instrument calibrations. However, acquisition geometry changed during this cruise. Refer to Figures 1 and 2 included with this archive (Data Series 237) for diagrams of acquisition geometry.

How can someone get a copy of the data set?

Are there legal restrictions on access or use of the data?
Access_Constraints: None. These data are held in the public domain.
Use_Constraints:
The U.S. Geological Survey and the University of New Orleans request to be acknowledged as originators of the data in future products or derivative research.
  1. Who distributes the data set? (Distributor 1 of 1)
    Shawn Dadisman
    U.S. Geological Survey
    Geologist
    600 4th Street South
    St. Petersburg, FL
    USA

    (727) 803-8747, ext. 3029 (voice)
    sdadisman@usgs.gov
    Contact_Instructions:
    Data may be available on-line only by special arrangement with the distributor above.
  2. What's the catalog number I need to order this data set? U.S. Geological Survey Data Series 237
  3. What legal disclaimers am I supposed to read?
    This DVD publication was prepared by an agency of the United States Government. Neither the United States Government nor any agency thereof nor any of their employees makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. Although all data and software published on this DVD have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software. The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the USGS in the use of these data, software, or related materials.
  4. How can I download or order the data?
    • Availability in digital form:
      Data format: The SEG-Y standard format (Barry and others, 1975) consists of the following: a 3,600-byte reel identification header, with the first 3,200 bytes consisting of an ASCII header block followed by a 400-byte binary header block, both of which include information specific to line and reel number; a trace data block that follows the reel identification header, with the first 240 bytes of each trace block consisting of the binary trace identification header; and seismic data samples that follow the trace identification header. in format SEG-Y Size: 9180
      Media you can order: DVD (format ISO 9660)
      Note: UNIX, LINUX, DOS, Macintosh
      Data format: The GIS project used to create the trackline maps is composed of map documents, shapefiles, and metadata. Map documents were created with ESRI ArcGIS 8.3 software. The shapefiles provided may also be viewed using other versions of ArcView, ArcGIS, or public domain software ArcExplorer (http://www.esri.com/software/arcexplorer/index.html). in format map document, shapefile, metadata Size: 23.1
      Network links: DVD/software/arc/arc.zip
      Data format: The SEG-Y standard format (Barry and others, 1975) consists of the following: a 3,600-byte reel identification header, with the first 3,200 bytes consisting of an ASCII header block followed by a 400-byte binary header block, both of which include information specific to line and reel number; a trace data block that follows the reel identification header, with the first 240 bytes of each trace block consisting of the binary trace identification header; and seismic data samples that follow the trace identification header. in format SEG-Y data download Size: 9180
      Network links: https://cmgds.marine.usgs.gov/data/04scc01/boomer/
      https://cmgds.marine.usgs.gov/data/04scc01/chirp/
    • Cost to order the data: Prices vary.

    • Special instructions:
      Publications are available from USGS Information Services, Box 25286, Federal Center, Denver, CO 80225-0046 (telephone: 1-888-ASK-USGS, e-mail: infoservices@usgs.gov).
  5. What hardware or software do I need in order to use the data set?
    Use of SEG-Y data requires specialized seismic processing software, such as public domain software Seismic Unix (http://www.cwp.mines.edu/cwpcodes/index.html).

Who wrote the metadata?

Dates:
Last modified: 13-Oct-2020
Metadata author:
Arnell Harrison
ETI, contracted by USGS
600 4th Street South
St. Petersburg, FL
USA

(727) 803-8747, ext. 3111 (voice)
aharrison@usgs.gov
Metadata standard:
Content Standard for Digital Geospatial Metadata (FGDC-STD-001-1998)
This page is <https://cmgds.marine.usgs.gov/catalog/spcmsc/ds-237metadata.faq.html>
Generated by mp version 2.9.50 on Tue Sep 21 18:18:53 2021