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ICDP drilling of the Eger Rift observatory: magmatic fluids driving the earthquake swarms and deep biosphere

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F22%3A00563123" target="_blank" >RIV/67985530:_____/22:00563123 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/22:10454715

  • Result on the web

    <a href="https://sd.copernicus.org/articles/31/31/2022/" target="_blank" >https://sd.copernicus.org/articles/31/31/2022/</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/sd-31-31-2022" target="_blank" >10.5194/sd-31-31-2022</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    ICDP drilling of the Eger Rift observatory: magmatic fluids driving the earthquake swarms and deep biosphere

  • Original language description

    The new in situ geodynamic laboratory established in the framework of the ICDP Eger project aims to develop the most modern, comprehensive, multiparameter laboratory at depth for studying earthquake swarms, crustal fluid flow, mantle-derived CO2 and helium degassing, and processes of the deep biosphere. In order to reach a new level of high-frequency, near-source and multiparameter observation of earthquake swarms and related phenomena, such a laboratory comprises a set of shallow boreholes with high-frequency 3-D seismic arrays as well as modern continuous real-time fluid monitoring at depth and the study of the deep biosphere. This laboratory is located in the western part of the Eger Rift at the border of the Czech Republic and Germany (in the West Bohemia-Vogtland geodynamic region) and comprises a set of five boreholes around the seismoactive zone. To date, all monitoring boreholes have been drilled. This includes the seismic monitoring boreholes S1, S2 and S3 in the crystalline units north and east of the major Nový Kostel seismogenic zone, borehole F3 in the Hartoušov mofette field and borehole S4 in the newly discovered Bažina maar near Libá. Supplementary borehole P1 is being prepared in the Neualbenreuth maar for paleoclimate and biological research. At each of these sites, a borehole broadband seismometer will be installed, and sites S1, S2 and S3 will also host a 3-D seismic array composed of a vertical geophone chain and surface seismic array. Seismic instrumenting has been completed in the S1 borehole and is in preparation in the remaining four monitoring boreholes. The continuous fluid monitoring site of Hartoušov includes three boreholes, F1, F2 and F3, and a pilot monitoring phase is underway. The laboratory also enables one to analyze microbial activity at CO2 mofettes and maar structures in the context of changes in habitats. The drillings into the maar volcanoes contribute to a better understanding of the Quaternary paleoclimate and volcanic activity.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10507 - Volcanology

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2022

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Scientific Drilling

  • ISSN

    1816-8957

  • e-ISSN

    1816-3459

  • Volume of the periodical

    31

  • Issue of the periodical within the volume

    October

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    19

  • Pages from-to

    31-49

  • UT code for WoS article

    000874498500001

  • EID of the result in the Scopus database

    2-s2.0-85141934520