search DOI 10.17882/48324

ODEMAR shipboard Pourquoi Pas? multibeam bathymetry

Multibeam bathymetry data, gridded at 40m, acquired around the 13°20'N and 13°30'N oceanic detachments along the Mid-Atlantic Ridge. Bathymetric data was acquired by the PourQUoi Pas? multibeam system (RESON 7150).

Data is provided as a grid in GRD format (GMT NETCDF).

grdinfo of the file:

  • ODEMAR_Shipboard_Bathymetry_40m.grd: Title: Bathy_40m.grd
  • ODEMAR_Shipboard_Bathymetry_40m.grd: Command: File written by MATLAB function grdwrite2.m
  • ODEMAR_Shipboard_Bathymetry_40m.grd: Remark: Created 22-Nov-2014 16:35:13
  • ODEMAR_Shipboard_Bathymetry_40m.grd: Gridline node registration used [Cartesian grid]
  • ODEMAR_Shipboard_Bathymetry_40m.grd: Grid file format: nf = GMT netCDF format (32-bit float), COARDS, CF-1.5
  • ODEMAR_Shipboard_Bathymetry_40m.grd: x_min: -45.14293893 x_max: -44.77177893 x_inc: 0.00036 name: x nx: 1032
  • ODEMAR_Shipboard_Bathymetry_40m.grd: y_min: 13.20017553 y_max: 13.62389553 y_inc: 0.00036 name: y ny: 1178
  • ODEMAR_Shipboard_Bathymetry_40m.grd: z_min: -4498.29248047 z_max: -1935.33117676 name: z
  • ODEMAR_Shipboard_Bathymetry_40m.grd: scale_factor: 1 add_offset: 0
  • ODEMAR_Shipboard_Bathymetry_40m.grd: format: classic

Disciplines

Marine geology

Keywords

Bathymetry, Mid-Ocean Ridge, Oceanic detachment, Fault, Core complex, Tectonics, Bathymetry, Mid-Atlantic Ridge

Location

13.5N, 13.33S, -44.8E, -45W

Data

FileSizeFormatProcessingAccess
Bathymetry grid - ODEMAR cruise
4 MoGMT NETCDFProcessed data
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How to cite
Escartin Javier (2017). ODEMAR shipboard Pourquoi Pas? multibeam bathymetry. SEANOE. https://doi.org/10.17882/48324
In addition to properly cite this dataset, it would be appreciated that the following work(s) be cited too, when using this dataset in a publication :
Escartin J., Mevel C., Petersen S., Bonnemains D., Cannat M., Andreani M., Augustin N., Bezos A., Chavagnac V., Choi Y., Godard M., Haaga K., Hamelin C., Ildefonse B., Jamieson J., John B., Leleu T., Macleod C. J., Massot-Campos M., Nomikou P., Olive J. A., Paquet M., Rommevaux C., Rothenbeck M., Steinfuhrer A., Tominaga M., Triebe L., Campos R., Gracias N., Garcia R. (2017). Tectonic structure, evolution, and the nature of oceanic core complexes and their detachment fault zones (13°20'N and 13°30'N, Mid-Atlantic Ridge). Geochemistry Geophysics Geosystems. 18 (4). 1451-1482. https://doi.org/10.1002/2016GC006775, https://archimer.ifremer.fr/doc/00376/48702/

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Oceanographic cruises
ODEMAR
Related documents
Verlaguet A., Bonnemains D., Mével C, Escartín J., Andreani M., Bourdelle F., Boiron M.‐C., Chavagnac V. (2021). Fluid circulation along an oceanic detachment fault: insights from fluid inclusions in silicified brecciated fault rocks (Mid‐Atlantic Ridge at 13°20’N). Geochemistry Geophysics Geosystems. 22 (1). e2020GC009235 (32p.). https://doi.org/10.1029/2020GC009235, https://archimer.ifremer.fr/doc/00661/77301/
Bonnemains D., Escartin J., Mevel C, Andreani M., Verlaguet A. (2017). Pervasive silicification and hanging wall overplating along the 13°20'N oceanic detachment fault (Mid-Atlantic Ridge). Geochemistry Geophysics Geosystems. 18 (6). 2028-2053. https://doi.org/10.1002/2017GC006846
Escartin J., Mevel C., Petersen S., Bonnemains D., Cannat M., Andreani M., Augustin N., Bezos A., Chavagnac V., Choi Y., Godard M., Haaga K., Hamelin C., Ildefonse B., Jamieson J., John B., Leleu T., Macleod C. J., Massot-Campos M., Nomikou P., Olive J. A., Paquet M., Rommevaux C., Rothenbeck M., Steinfuhrer A., Tominaga M., Triebe L., Campos R., Gracias N., Garcia R. (2017). Tectonic structure, evolution, and the nature of oceanic core complexes and their detachment fault zones (13°20'N and 13°30'N, Mid-Atlantic Ridge). Geochemistry Geophysics Geosystems. 18 (4). 1451-1482. https://doi.org/10.1002/2016GC006775, https://archimer.ifremer.fr/doc/00376/48702/
Related datasets
Escartin Javier (2023). Transit shipboard bathymetry from the ODEMAR cruise (Pourquoi Pas?, 2013). SEANOE. https://doi.org/10.17882/97230
Escartín Javier, Petersen Sven (2017). ODEMAR AUV Abyss (GEOMAR) + shipboard Pourquoi Pas? multibeam bathymetry - 13deg20'N and 13deg30'N Oceanic Core Complexes, Mid Atlantic Ridge. SEANOE. https://doi.org/10.17882/48335
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