urn:ieda:metadata:for:doi:10.14470/4P7565788335
eng
dataset
Seismic Network
Interdisciplinary Earth Data Alliance | Lamont Doherty Earth
Observatory | Columbia Univeristy
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pointOfContact
ISO 19139 Geographic Information - Metadata - Implementation Specification
2007
urn:ogc:def:crs:EPSG:4326
High Resolution Seismological Profiling across Sierra Nevada (HIRE)
2015-12-22
creation
2010
publication
doi:10.14470/4P7565788335
Heit, Benjamin
missing@unknown.org
author
Yuan, Xiaohui
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author
Mancilla, Flor De Lis
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author
Deutsches GeoForschungsZentrum GFZ
HostingInstitution
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distributor
GEOFON Data Centre
DataCollector
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collaborator
GEOFON Data Centre
Distributor
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originator
GEOFON Data Centre
DataManager
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custodian
Geofon@Gfz-Potsdam.De
ContactPerson
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pointOfContact
Geophysical Instrument Pool Potsdam (GIPP)
Sponsor
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funder
Deutsches GeoForschungsZentrum GFZ
ProjectLeader
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collaborator
Deutsches GeoForschungsZentrum GFZ
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publisher
Abstract: We operated a densely spaced broadband seismic field experiment to study the structure of the crust and mantle lithosphere across the Sierra Nevada mountain range, southern Spain. The Sierra Nevada is one of the key areas within the complicated Betic-Alboran-Rif system. It contains the highest mountain of the Iberian Peninsula and is located in the close vicinity of a very deep seismic zone (>600 km depth). This region plays a decisive role in answering the question if subduction or delamination is the dominant geological process in the western Mediterranean. The seismic array, consisting of 40 broadband stations spaced 2 km apart (compared to earlier station spacing of ~50 km), has been deployed in September 2010 by a joint effort of GFZ Potsdam and University of Granada, and has
been operated until the end of 2011. The proposed scientific work is the analysis of the data collected with the present experiment which includes mainly P and S receiver function analysis and surface wave tomography with ambient noise data. We will image the seismic structure and thickness variation of the crust and mantle lithosphere at high resolution and hence infer tectonic and geodynamic processes related to the Africa-Eurasia collision. The resulting structural details especially of the mantle lithosphere will contribute essentially to the recognition of the geodynamic deformations in the western part of the African-Eurasian plate collision. Data are available from the GFZ seismological data archive.
funderName:Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ
funderIdentifier:https://doi.org/10.13039/501100010956; IDType:Crossref Funder ID
awardNumber:GIPP201016
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/9C/2010_2011
URL
HasMetadata
eng
-3.1
-2.9
36.7
37.3
Spain
2010-06-29
2011-12-31
390000000000
http://dx.doi.org/10.14470/4P7565788335
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Stephen M. Richard
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