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author Marjanovic, Milena
Satish, Singh
Grevemeyer, Ingo
author_facet Marjanovic, Milena
Satish, Singh
Grevemeyer, Ingo
collection Datos científicos de ciencias marinas y ambientales
contents These dataset was collected in the equatorial Atlantic during ILAB-SPARC experiment conducted aboard N/O Pourquoi Pas? in Fall 2018. The seismic data sample the oceanic lithosphere extending between the Romanche Transform Fault to the Charcot Fracture Zone. Refraction data were collected during the ILAB-SPARC experiment. The provided refraction data were recorded on 25 Ocean Bottom Seismometer (OBS data) instruments (from 25 to 50) and span source-receiver offsets from ~-100 km to 100 km. Finally, we provide our final velocity model obtained by analyzing the OBS data (the data are provided in ascii format (horizontal and vertical grid sizes are 200 m and 50 m, respectively).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_922330
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Seismic refraction datasets and velocity model during cruise ILAB-SPARC, Chain Fracture Zone
Marjanovic, Milena
Satish, Singh
Grevemeyer, Ingo
Binary Object; Binary Object (File Size); Equatorial Atlantic; Event label; ILAB-SPARC; ILAB-SPARC_OBS_26; ILAB-SPARC_OBS_27; ILAB-SPARC_OBS_28; ILAB-SPARC_OBS_29; ILAB-SPARC_OBS_30; ILAB-SPARC_OBS_31; ILAB-SPARC_OBS_32; ILAB-SPARC_OBS_33; ILAB-SPARC_OBS_34; ILAB-SPARC_OBS_35; ILAB-SPARC_OBS_36; ILAB-SPARC_OBS_37; ILAB-SPARC_OBS_38; ILAB-SPARC_OBS_39; ILAB-SPARC_OBS_40; ILAB-SPARC_OBS_41; ILAB-SPARC_OBS_42; ILAB-SPARC_OBS_43; ILAB-SPARC_OBS_44; ILAB-SPARC_OBS_45; ILAB-SPARC_OBS_46; ILAB-SPARC_OBS_47; ILAB-SPARC_OBS_48; ILAB-SPARC_OBS_49; ILAB-SPARC_OBS_50; OBS; Ocean bottom seismometer; Pourquoi Pas ? (2005)
These dataset was collected in the equatorial Atlantic during ILAB-SPARC experiment conducted aboard N/O Pourquoi Pas? in Fall 2018. The seismic data sample the oceanic lithosphere extending between the Romanche Transform Fault to the Charcot Fracture Zone. Refraction data were collected during the ILAB-SPARC experiment. The provided refraction data were recorded on 25 Ocean Bottom Seismometer (OBS data) instruments (from 25 to 50) and span source-receiver offsets from ~-100 km to 100 km. Finally, we provide our final velocity model obtained by analyzing the OBS data (the data are provided in ascii format (horizontal and vertical grid sizes are 200 m and 50 m, respectively).
title Seismic refraction datasets and velocity model during cruise ILAB-SPARC, Chain Fracture Zone
topic Binary Object; Binary Object (File Size); Equatorial Atlantic; Event label; ILAB-SPARC; ILAB-SPARC_OBS_26; ILAB-SPARC_OBS_27; ILAB-SPARC_OBS_28; ILAB-SPARC_OBS_29; ILAB-SPARC_OBS_30; ILAB-SPARC_OBS_31; ILAB-SPARC_OBS_32; ILAB-SPARC_OBS_33; ILAB-SPARC_OBS_34; ILAB-SPARC_OBS_35; ILAB-SPARC_OBS_36; ILAB-SPARC_OBS_37; ILAB-SPARC_OBS_38; ILAB-SPARC_OBS_39; ILAB-SPARC_OBS_40; ILAB-SPARC_OBS_41; ILAB-SPARC_OBS_42; ILAB-SPARC_OBS_43; ILAB-SPARC_OBS_44; ILAB-SPARC_OBS_45; ILAB-SPARC_OBS_46; ILAB-SPARC_OBS_47; ILAB-SPARC_OBS_48; ILAB-SPARC_OBS_49; ILAB-SPARC_OBS_50; OBS; Ocean bottom seismometer; Pourquoi Pas ? (2005)
url https://doi.org/10.1594/PANGAEA.922330