Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997)

This 1997 Ewing expedition to the Mid-Atlantic Ridge, part of the Nobel at the Mid-Atlantic Ridge Seismic Experiment, collected ocean bottom seismic refraction and single-channel seismic data. The purpose was to measure the reflected and refracted arrivals of seismic energy from sections of the mid-...

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Main Authors: Collins, John, Blackman, Donna, Lemmond, Peter
Format: Dataset
Language:English
Published: Interdisciplinary Earth Data Alliance (IEDA) 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/ieda/500133
http://doi.iedadata.org/500133
id ftdatacite:10.1594/ieda/500133
record_format openpolar
spelling ftdatacite:10.1594/ieda/500133 2023-05-15T17:32:13+02:00 Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997) Collins, John Blackman, Donna Lemmond, Peter 2018 application/seismic-segy, text/plain, image/gif https://dx.doi.org/10.1594/ieda/500133 http://doi.iedadata.org/500133 en eng Interdisciplinary Earth Data Alliance (IEDA) http://www.marine-geo.org/tools/search/entry.php?id=EW9704 http://www.marine-geo.org/tools/search/entry.php?id=EW9704 https://dx.doi.org/10.1029/2008gc002121 https://dx.doi.org/10.1029/2010gl045165 Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC BY-NC-SA 3.0] http://creativecommons.org/licenses/by-nc-sa/3.0/us CC-BY-NC-SA Marine Geoscience Oceans Solid Earth Seismic Refraction Spreading Center SeismicActiveOBS EW9704 Maurice Ewing North Atlantic ridge, Mid-Atlantic ridge, slow spreading, Kane Fracture Zone, NOMAR dataset Dataset 2018 ftdatacite https://doi.org/10.1594/ieda/500133 https://doi.org/10.1029/2008gc002121 https://doi.org/10.1029/2010gl045165 2021-11-05T12:55:41Z This 1997 Ewing expedition to the Mid-Atlantic Ridge, part of the Nobel at the Mid-Atlantic Ridge Seismic Experiment, collected ocean bottom seismic refraction and single-channel seismic data. The purpose was to measure the reflected and refracted arrivals of seismic energy from sections of the mid-ocean ridge spreading center which have known, previously sampled, rock compositions. These data could then be used to identify and map rock types and test existing models for subsurface ridge structure, possibly providing a 3-dimensional map of the structure of a slow-spreading mid-ocean ridge. Funded by NSF grant OCE96-33114. Dataset North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Mid-Atlantic Ridge Maurice ENVELOPE(-55.817,-55.817,-63.133,-63.133) Kane ENVELOPE(-63.038,-63.038,-73.952,-73.952) Ewing ENVELOPE(-61.257,-61.257,-69.924,-69.924)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Marine Geoscience
Oceans
Solid Earth
Seismic Refraction
Spreading Center
SeismicActiveOBS
EW9704
Maurice Ewing
North Atlantic
ridge, Mid-Atlantic ridge, slow spreading, Kane Fracture Zone, NOMAR
spellingShingle Marine Geoscience
Oceans
Solid Earth
Seismic Refraction
Spreading Center
SeismicActiveOBS
EW9704
Maurice Ewing
North Atlantic
ridge, Mid-Atlantic ridge, slow spreading, Kane Fracture Zone, NOMAR
Collins, John
Blackman, Donna
Lemmond, Peter
Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997)
topic_facet Marine Geoscience
Oceans
Solid Earth
Seismic Refraction
Spreading Center
SeismicActiveOBS
EW9704
Maurice Ewing
North Atlantic
ridge, Mid-Atlantic ridge, slow spreading, Kane Fracture Zone, NOMAR
description This 1997 Ewing expedition to the Mid-Atlantic Ridge, part of the Nobel at the Mid-Atlantic Ridge Seismic Experiment, collected ocean bottom seismic refraction and single-channel seismic data. The purpose was to measure the reflected and refracted arrivals of seismic energy from sections of the mid-ocean ridge spreading center which have known, previously sampled, rock compositions. These data could then be used to identify and map rock types and test existing models for subsurface ridge structure, possibly providing a 3-dimensional map of the structure of a slow-spreading mid-ocean ridge. Funded by NSF grant OCE96-33114.
format Dataset
author Collins, John
Blackman, Donna
Lemmond, Peter
author_facet Collins, John
Blackman, Donna
Lemmond, Peter
author_sort Collins, John
title Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997)
title_short Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997)
title_full Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997)
title_fullStr Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997)
title_full_unstemmed Ocean bottom seismometer (OBS) data on the Mid-Atlantic Ridge, acquired during the R/V Maurice Ewing survey EW9704 (1997)
title_sort ocean bottom seismometer (obs) data on the mid-atlantic ridge, acquired during the r/v maurice ewing survey ew9704 (1997)
publisher Interdisciplinary Earth Data Alliance (IEDA)
publishDate 2018
url https://dx.doi.org/10.1594/ieda/500133
http://doi.iedadata.org/500133
long_lat ENVELOPE(-55.817,-55.817,-63.133,-63.133)
ENVELOPE(-63.038,-63.038,-73.952,-73.952)
ENVELOPE(-61.257,-61.257,-69.924,-69.924)
geographic Mid-Atlantic Ridge
Maurice
Kane
Ewing
geographic_facet Mid-Atlantic Ridge
Maurice
Kane
Ewing
genre North Atlantic
genre_facet North Atlantic
op_relation http://www.marine-geo.org/tools/search/entry.php?id=EW9704
http://www.marine-geo.org/tools/search/entry.php?id=EW9704
https://dx.doi.org/10.1029/2008gc002121
https://dx.doi.org/10.1029/2010gl045165
op_rights Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC BY-NC-SA 3.0]
http://creativecommons.org/licenses/by-nc-sa/3.0/us
op_rightsnorm CC-BY-NC-SA
op_doi https://doi.org/10.1594/ieda/500133
https://doi.org/10.1029/2008gc002121
https://doi.org/10.1029/2010gl045165
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