Seismic refraction and wide-angle data surveying the continent-to-ocean transition zone in the Iberia Abyssal Plain

Fuente: PANGAEA
Salvato in:
Dettagli Bibliografici
Autori principali: Grevemeyer, Ingo, Ranero, César R, Sallarès, Valenti
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2022
Soggetti:
Accesso online:
Tags: Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
_version_ 1867170112507740160
author Grevemeyer, Ingo
Ranero, César R
Sallarès, Valenti
author_facet Grevemeyer, Ingo
Ranero, César R
Sallarès, Valenti
collection Datos científicos de ciencias marinas y ambientales
contents In September of 2018, the Spanish research vessel Sarmiento de Gamboa shot the seismic profile FRAME-p03 across the continent-to-ocean transition zone in the Iberia Abyssal Plain of the Western Iberia passive continental margion to the west of Portugal. Seismic shots were recorded on 30 ocean-bottom-seismometers (OBS) and ocean-bottom-hydrophones (OBH). Spanish instruments were OBS from the Spanish Pool operated by the Marine Technology Unit (UTM) of Consejo Superior de Investigaciones Científicas (CSIC) and German istruments were OBH from the GEOMAR Helmholtz Centre for Ocean Research Kiel. Seismic data in SEGY format of the all seismic stations of both partners are archived at the PANGAEA Datacenter. Please note that the data have a time offset of 1 sec and a reduction velocity of 8 km/s. The seismic FRAME (Formation of Geological Domains in the Western Iberian Margin and Tectonic Reactivation of their Limit) cruise was funded by the Spanish Ministry of Science.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_941102
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Seismic refraction and wide-angle data surveying the continent-to-ocean transition zone in the Iberia Abyssal Plain
Grevemeyer, Ingo
Ranero, César R
Sallarès, Valenti
Atlantic; Binary Object; Binary Object (File Size); Elevation of event; Event label; File content; FRAME-OBS; FRAME-OBS_OBH100; FRAME-OBS_OBH101; FRAME-OBS_OBH102; FRAME-OBS_OBH103; FRAME-OBS_OBH76; FRAME-OBS_OBH77; FRAME-OBS_OBH78; FRAME-OBS_OBH79; FRAME-OBS_OBH80; FRAME-OBS_OBH81; FRAME-OBS_OBH88; FRAME-OBS_OBH89; FRAME-OBS_OBH90; FRAME-OBS_OBH91; FRAME-OBS_OBH92; FRAME-OBS_OBH93; FRAME-OBS_OBS104; FRAME-OBS_OBS105; FRAME-OBS_OBS82; FRAME-OBS_OBS83; FRAME-OBS_OBS84; FRAME-OBS_OBS85; FRAME-OBS_OBS86; FRAME-OBS_OBS87; FRAME-OBS_OBS94; FRAME-OBS_OBS95; FRAME-OBS_OBS96; FRAME-OBS_OBS97; FRAME-OBS_OBS98; FRAME-OBS_OBS99; FRAME-OBS_P03; Latitude of event; Longitude of event; North Atlantic Ocean; OBH; OBS; Ocean bottom hydrophone; ocean-bottom-hydrophones; ocean bottom seismometer; Ocean bottom seismometer; oceanic crust; passive continental margin; Portuguese Margin; S03; Sarmiento de Gamboa; seismic data; Seismic refraction profile; SEISREFR
In September of 2018, the Spanish research vessel Sarmiento de Gamboa shot the seismic profile FRAME-p03 across the continent-to-ocean transition zone in the Iberia Abyssal Plain of the Western Iberia passive continental margion to the west of Portugal. Seismic shots were recorded on 30 ocean-bottom-seismometers (OBS) and ocean-bottom-hydrophones (OBH). Spanish instruments were OBS from the Spanish Pool operated by the Marine Technology Unit (UTM) of Consejo Superior de Investigaciones Científicas (CSIC) and German istruments were OBH from the GEOMAR Helmholtz Centre for Ocean Research Kiel. Seismic data in SEGY format of the all seismic stations of both partners are archived at the PANGAEA Datacenter. Please note that the data have a time offset of 1 sec and a reduction velocity of 8 km/s. The seismic FRAME (Formation of Geological Domains in the Western Iberian Margin and Tectonic Reactivation of their Limit) cruise was funded by the Spanish Ministry of Science.
title Seismic refraction and wide-angle data surveying the continent-to-ocean transition zone in the Iberia Abyssal Plain
topic Atlantic; Binary Object; Binary Object (File Size); Elevation of event; Event label; File content; FRAME-OBS; FRAME-OBS_OBH100; FRAME-OBS_OBH101; FRAME-OBS_OBH102; FRAME-OBS_OBH103; FRAME-OBS_OBH76; FRAME-OBS_OBH77; FRAME-OBS_OBH78; FRAME-OBS_OBH79; FRAME-OBS_OBH80; FRAME-OBS_OBH81; FRAME-OBS_OBH88; FRAME-OBS_OBH89; FRAME-OBS_OBH90; FRAME-OBS_OBH91; FRAME-OBS_OBH92; FRAME-OBS_OBH93; FRAME-OBS_OBS104; FRAME-OBS_OBS105; FRAME-OBS_OBS82; FRAME-OBS_OBS83; FRAME-OBS_OBS84; FRAME-OBS_OBS85; FRAME-OBS_OBS86; FRAME-OBS_OBS87; FRAME-OBS_OBS94; FRAME-OBS_OBS95; FRAME-OBS_OBS96; FRAME-OBS_OBS97; FRAME-OBS_OBS98; FRAME-OBS_OBS99; FRAME-OBS_P03; Latitude of event; Longitude of event; North Atlantic Ocean; OBH; OBS; Ocean bottom hydrophone; ocean-bottom-hydrophones; ocean bottom seismometer; Ocean bottom seismometer; oceanic crust; passive continental margin; Portuguese Margin; S03; Sarmiento de Gamboa; seismic data; Seismic refraction profile; SEISREFR
url https://doi.org/10.1594/PANGAEA.941102