2026-08-05T03:23:16Zhttp://doidb.wdc-terra.org/oaip/oai

oai:doidb.wdc-terra.org:67992025-01-27T15:59:07ZDOIDBDOIDB.SEISNET

false4DOIDB.SEISNET 10.14470/MJ7559637482 Rietbrock, Andreas Haberland, Christian Bataille, Klaus Lange, Dietrich Dahm, Torsten GFZ Data Services 2004 Deutsches GeoForschungsZentrum GFZ GEOFON Data Centre geofon@gfz.de Universidad de Concepción Geophysical Instrument Pool Potsdam (GIPP) Deutsches GeoForschungsZentrum GFZ EARTH SCIENCE > SOLID EARTH > TECTONICS > EARTHQUAKES In Situ/Laboratory Instruments > Magnetic/Motion Sensors > Seismometers In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS > SEISMOLOGICAL STATIONS Monitoring system Seismological stations Passive seismic Seismometers Velocity MiniSEED GIPP MESI Geophysics Temporary 2004-01-01 2004-01-01 2020-01-16 2004-01-01 en Seismic Network Creative Commons Attribution 4.0 International https://geofon.gfz.de/waveform/archive/response/ZW/2004_2005 507.3GB .mseed XML Understanding the factors leading to large earthquakes in the coupling zone of convergent margins and their interrelation with surface deformation were the main aims of the international and interdisciplinary research initiative TIPTEQ (“From The Incoming Plate To megaThrust EarthQuake Processes”). Between Nov. 2004 and Oct. 2005 we deployed 2 temporary, amphibious seismic arrays in South-Central Chile. In this region the 1960 Mw = 9.5 earthquake nucleated. The northern network between 37° and 39°S was formed by up to 120 digitally recording land stations (equipped with short-period sensors) and 10 Ocean Bottom Seismometers/Hydrophones (OBS/OBH). Waveform data are available from the GEOFON data centre, under network code ZW, and are available under CC-BY 4.0 license according to GIPP-rules. -73.9 -71.4 -39.3 -37.0 Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ https://doi.org/10.13039/501100010956 GIPP200404