2026-05-17T15:55:12Zhttp://doidb.wdc-terra.org/oaip/oai

oai:doidb.wdc-terra.org:69312025-08-18T12:12:29ZDOIDBDOIDB.SEISNET

false4DOIDB.SEISNET 10.14470/4W7564850022 Reiss, Miriam Christina 0000-0002-0250-4988 Goethe University, Frankfurt am Main Rümpker, Georg 0000-0002-5348-9888 Goethe Universität, Frankfurt am Main, Germany GFZ Data Services 2020 Deutsches GeoForschungsZentrum GFZ GEOFON Data Centre geofon@gfz.de Geophysical Instrument Pool Potsdam (GIPP) Deutsches GeoForschungsZentrum GFZ Monitoring system Seismological stations In Situ/Laboratory Instruments > Magnetic/Motion Sensors > Seismometers In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS EARTH SCIENCE > SOLID EARTH > TECTONICS > VOLCANIC ACTIVITY Geophysics Passive seismic Seismometers Velocity MiniSEED Volcano Temporary GIPP MESI 2019-01-01 2020-02-01 2020-09-28 2020-09-28 2025-11-01 en Seismic Network https://geofon.gfz.de/waveform/archive/response/9J/2019_2020 embargoed access Creative Commons Attribution 4.0 International 218GB .mseed XML Oldoinyo Lengai in the North Tanzanian Divergence is the only active natrocarbonatite volcano world-wide and presents an important endmember magmatic system in a young rift segment of the East African Rift System. This volcano typically experiences long-duration episodes of natrocarbonatitic effusions with intermittent short-duration explosive eruptions. To better understand the role of the stress interactions and magma plumbing on the eruptions dynamics, this study aims to constrain the subsurface magmatic architecture of Oldoinyo Lengai, and a zone of ongoing seismicity and intrusive activity below the extinct 1 Ma-old Gelai shield volcano and active Naibor Soito monogenetic cone field. Waveform data are available from the GEOFON data centre, under network code 9J. 35.0 37.0 -3.0 -2.0 Tanzania Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ https://doi.org/10.13039/501100010956 GIPP201901 Deutsche Forschungsgemeinschaft (DFG) RE 4321/1-1