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Trans-crustal structural control of CO2-rich extensional magmatic systems revealed at Mount Erebus Antarctica

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F22%3A00558416" target="_blank" >RIV/67985530:_____/22:00558416 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.nature.com/articles/s41467-022-30627-7" target="_blank" >https://www.nature.com/articles/s41467-022-30627-7</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1038/s41467-022-30627-7" target="_blank" >10.1038/s41467-022-30627-7</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Trans-crustal structural control of CO2-rich extensional magmatic systems revealed at Mount Erebus Antarctica

  • Original language description

    Erebus volcano, Antarctica, with its persistent phonolite lava lake, is a classic example of an evolved, CO2-rich rift volcano. Seismic studies provide limited images of the magmatic system. Here we show using magnetotelluric data that a steep, melt-related conduit of low electrical resistivity originating in the upper mantle undergoes pronounced lateral re-orientation in the deep crust before reaching shallower magmatic storage and the summit lava lake. The lateral turn represents a structural fault-valve controlling episodic flow of magma and CO2 vapour, which replenish and heat the high level phonolite differentiation zone. This magmatic valve lies within an inferred, east-west structural trend forming part of an accommodation zone across the southern termination of the Terror Rift, providing a dilatant magma pathway. Unlike H2O-rich subduction arc volcanoes, CO2-dominated Erebus geophysically shows continuous magmatic structure to shallow crustal depths of < 1 km, as the melt does not experience decompression-related volatile supersaturation and viscous stalling.

  • 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

  • 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

    Nature Communications

  • ISSN

    2041-1723

  • e-ISSN

    2041-1723

  • Volume of the periodical

    13

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    10

  • Pages from-to

    2989

  • UT code for WoS article

    000805647600024

  • EID of the result in the Scopus database

    2-s2.0-85130960852