urn:ieda:metadata:for:doi:10.14470/8U7561563769
eng
dataset
Seismic Network
Interdisciplinary Earth Data Alliance | Lamont Doherty Earth
Observatory | Columbia Univeristy
info@EarthChem.org
http://www.earthchem.org/sites/earthchem.org/files/arthemia_logo.jpg
logo
graphic
pointOfContact
ISO 19139 Geographic Information - Metadata - Implementation Specification
2007
urn:ogc:def:crs:EPSG:4326
Renland
2017-04-06
creation
2016
publication
doi:10.14470/8U7561563769
Larose, Eric
missing@unknown.org
author
Deutsches GeoForschungsZentrum GFZ
HostingInstitution
missing@unknown.org
distributor
GEOFON Data Centre
DataCollector
missing@unknown.org
collaborator
GEOFON Data Centre
Distributor
missing@unknown.org
originator
GEOFON Data Centre
DataManager
missing@unknown.org
custodian
Geofon@Gfz-Potsdam.De
ContactPerson
missing@unknown.org
pointOfContact
Geophysical Instrument Pool Potsdam (GIPP)
Sponsor
missing@unknown.org
funder
ISTerre, Université Grenoble Alpes, CNRS (ISTerre)
ProjectLeader
missing@unknown.org
collaborator
GFZ Data Services
missing@unknown.org
publisher
Abstract: The experiments are performed down the Edward Bailey valley, in the Renland peninsula, Scoresby Sund, Greenland. General purpose: ambient seismic noise recordings are obtained to characterize the geometry/structure of the valley the geometry/structure of the glaciers the microseismicity of the glacier, the friction process, crack orientation and mechanisms the seismic activity of glacial rivers, the relation between hydrological flow and noise spectrum the localization and characterization of sub-glacial flow from surface recordings. Seismic stations were composed of 3C broadband Trillium compact seismometer, a Cube datalogger and a 12V (D-cell types, stacked) battery pack.The experiment splits into three surveys performed at three different sites, one after the other, from july to august 2016. In the first experiment, we deploy 11 stations, 9 of them on a flat sandy area covering, partly, immobile ice that seems to be blocked between the Bailey Glacier (upstream) and the Apusinikajik glacier (downstream). The 9 sensors are placed a few hundreds of meters from the Apusinikajik lateral front, the last 2 are placed on the glacier next to the collapsing front. In the second and third experiment (chronologically speaking), we deploy 10 and 8 stations, respectively. Each deployment is performed along a Bailey valley transect. The first one intercepts the front-end of the glacier and the sub-glacial river exit (flow of several m3/s). The second transect is performed some 850m upstream. Waveform data are available from the GEOFON data centre, under network code 3H, and are embargoed until summer of 2019.
funderName:Naturevolution
funderName:Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ
funderIdentifier:https://doi.org/10.13039/501100010956; IDType:Crossref Funder ID
awardNumber:GIPP201614
Complete
Geofon@Gfz-Potsdam.De
ContactPerson
missing@unknown.org
pointOfContact
.mseed
Seismic waveforms
Monitoring system
GEMET - INSPIRE themes, version 1.0
publication
In Situ/Laboratory Instruments > Magnetic/Motion Sensors > Seismometers
GCMD Instruments
publication
In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS
GCMD Platforms
publication
https://creativecommons.org/licenses/by-nc-sa/4.0/legalcodeCreative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC BY-NC-SA 3.0]
https://geofon.gfz-potsdam.de/waveform/archive/response/3H/2016_2016
URL
HasMetadata
eng
71.2
71.3
-26
-25.9
Renland
2016-01-01
2016-12-31
30000000000
http://dx.doi.org/10.14470/8U7561563769
WWW:LINK-1.0-http--link
Landing Page
Link to DOI landing page or data facility landing page if no DOI is assigned.
information
This metadata record was generated by an xslt transformation from a DataCite metadata record;
The originator of the dataCite record should be cited in the metadataContact field of this record. The transform was
created by Damian Ulbricht and Stephen M. Richard. Run on 2024-03-29
Stephen M. Richard
info@iedadata.org
processor