Laptev Sea Rift Seismological Network (SIOLA) Part I ...
The Laptev Sea region is one of the very few places on Earth where mid-ocean spreading centres continue into continental rift zones. The Gakkel Ridge, the active spreading centre in the Eurasia Basin of the Arctic Ocean, is characterized by well-defined seismicity close to its axial graben. In contr...
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GFZ Data Services
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Online Access: | https://dx.doi.org/10.14470/3o7561738646 https://geofon.gfz-potsdam.de/doi/network/8B/2016 |
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ftdatacite:10.14470/3o7561738646 2024-03-31T07:50:53+00:00 Laptev Sea Rift Seismological Network (SIOLA) Part I ... Geissler, Wolfram Shibaev, Sergey Krüger, Frank Baranov, Boris Haberland, Christian Tsukanov, Nikolai Ploetz, Aline Vollmer, Daniel Pravkin, Sergey 2020 .mseed XML https://dx.doi.org/10.14470/3o7561738646 https://geofon.gfz-potsdam.de/doi/network/8B/2016 en eng GFZ Data Services https://geofon.gfz-potsdam.de/waveform/archive/response/8B/2016_2017 https://dx.doi.org/10.2312/bzpm_0709_2017 https://dx.doi.org/10.2312/bzpm_0725_2018 https://geofon.gfz-potsdam.de/waveform/archive/response/8B/2016_2017 Creative Commons Attribution 4.0 International embargoed access https://vocabularies.coar-repositories.org/access_rights/c_f1cf/ https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Broadband seismic waveforms Seismic monitoring temporary local seismic network Arctic Siberia continental rifting Laptev Sea Siberian Craton Verkhoyansk Fold-and-Thrust Belt Monitoring system EARTH SCIENCE > SOLID EARTH 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 dataset Seismic Network Dataset 2020 ftdatacite https://doi.org/10.14470/3o756173864610.2312/bzpm_0709_201710.2312/bzpm_0725_2018 2024-03-04T14:03:39Z The Laptev Sea region is one of the very few places on Earth where mid-ocean spreading centres continue into continental rift zones. The Gakkel Ridge, the active spreading centre in the Eurasia Basin of the Arctic Ocean, is characterized by well-defined seismicity close to its axial graben. In contrast below the Laptev Sea Shelf, which consists of a series of sediment filled grabens (500 km wide, 700 km long), only more diffuse seismic activity is observed. The pre-rift basement in the Laptev Sea is most probably formed by Late-Paleozoic and Late-Mesozoic fold belts. The Laptev Rift Basin is filled with Upper Cretaceous and Cenozoic sediments of variable thickness (1.5 to 14 km). The westernmost limit of seismicity is located close to edge of thick lithosphere of the Siberian Shield, which indicates some structural control on the recent tectonic activity. Focal depths are mainly less than 25 km (continent) and less than 10 km (ocean). Sparse observations of upper mantle earthquakes are under debate. The pole ... Dataset Arctic Arctic Ocean laptev Laptev Sea Siberia DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Eurasia Basin ENVELOPE(80.000,80.000,87.000,87.000) Gakkel Ridge ENVELOPE(90.000,90.000,87.000,87.000) Laptev Sea Verkhoyansk ENVELOPE(133.400,133.400,67.544,67.544) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Broadband seismic waveforms Seismic monitoring temporary local seismic network Arctic Siberia continental rifting Laptev Sea Siberian Craton Verkhoyansk Fold-and-Thrust Belt Monitoring system EARTH SCIENCE > SOLID EARTH 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 |
spellingShingle |
Broadband seismic waveforms Seismic monitoring temporary local seismic network Arctic Siberia continental rifting Laptev Sea Siberian Craton Verkhoyansk Fold-and-Thrust Belt Monitoring system EARTH SCIENCE > SOLID EARTH 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 Geissler, Wolfram Shibaev, Sergey Krüger, Frank Baranov, Boris Haberland, Christian Tsukanov, Nikolai Ploetz, Aline Vollmer, Daniel Pravkin, Sergey Laptev Sea Rift Seismological Network (SIOLA) Part I ... |
topic_facet |
Broadband seismic waveforms Seismic monitoring temporary local seismic network Arctic Siberia continental rifting Laptev Sea Siberian Craton Verkhoyansk Fold-and-Thrust Belt Monitoring system EARTH SCIENCE > SOLID EARTH 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 |
description |
The Laptev Sea region is one of the very few places on Earth where mid-ocean spreading centres continue into continental rift zones. The Gakkel Ridge, the active spreading centre in the Eurasia Basin of the Arctic Ocean, is characterized by well-defined seismicity close to its axial graben. In contrast below the Laptev Sea Shelf, which consists of a series of sediment filled grabens (500 km wide, 700 km long), only more diffuse seismic activity is observed. The pre-rift basement in the Laptev Sea is most probably formed by Late-Paleozoic and Late-Mesozoic fold belts. The Laptev Rift Basin is filled with Upper Cretaceous and Cenozoic sediments of variable thickness (1.5 to 14 km). The westernmost limit of seismicity is located close to edge of thick lithosphere of the Siberian Shield, which indicates some structural control on the recent tectonic activity. Focal depths are mainly less than 25 km (continent) and less than 10 km (ocean). Sparse observations of upper mantle earthquakes are under debate. The pole ... |
format |
Dataset |
author |
Geissler, Wolfram Shibaev, Sergey Krüger, Frank Baranov, Boris Haberland, Christian Tsukanov, Nikolai Ploetz, Aline Vollmer, Daniel Pravkin, Sergey |
author_facet |
Geissler, Wolfram Shibaev, Sergey Krüger, Frank Baranov, Boris Haberland, Christian Tsukanov, Nikolai Ploetz, Aline Vollmer, Daniel Pravkin, Sergey |
author_sort |
Geissler, Wolfram |
title |
Laptev Sea Rift Seismological Network (SIOLA) Part I ... |
title_short |
Laptev Sea Rift Seismological Network (SIOLA) Part I ... |
title_full |
Laptev Sea Rift Seismological Network (SIOLA) Part I ... |
title_fullStr |
Laptev Sea Rift Seismological Network (SIOLA) Part I ... |
title_full_unstemmed |
Laptev Sea Rift Seismological Network (SIOLA) Part I ... |
title_sort |
laptev sea rift seismological network (siola) part i ... |
publisher |
GFZ Data Services |
publishDate |
2020 |
url |
https://dx.doi.org/10.14470/3o7561738646 https://geofon.gfz-potsdam.de/doi/network/8B/2016 |
long_lat |
ENVELOPE(80.000,80.000,87.000,87.000) ENVELOPE(90.000,90.000,87.000,87.000) ENVELOPE(133.400,133.400,67.544,67.544) |
geographic |
Arctic Arctic Ocean Eurasia Basin Gakkel Ridge Laptev Sea Verkhoyansk |
geographic_facet |
Arctic Arctic Ocean Eurasia Basin Gakkel Ridge Laptev Sea Verkhoyansk |
genre |
Arctic Arctic Ocean laptev Laptev Sea Siberia |
genre_facet |
Arctic Arctic Ocean laptev Laptev Sea Siberia |
op_relation |
https://geofon.gfz-potsdam.de/waveform/archive/response/8B/2016_2017 https://dx.doi.org/10.2312/bzpm_0709_2017 https://dx.doi.org/10.2312/bzpm_0725_2018 https://geofon.gfz-potsdam.de/waveform/archive/response/8B/2016_2017 |
op_rights |
Creative Commons Attribution 4.0 International embargoed access https://vocabularies.coar-repositories.org/access_rights/c_f1cf/ https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.14470/3o756173864610.2312/bzpm_0709_201710.2312/bzpm_0725_2018 |
_version_ |
1795029361534959616 |