% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Menzel:908609,
      author       = {Menzel, Manuel D. and Urai, Janos L. and Ukar, Estibalitz
                      and Hirth, Greg and Schwedt, Alexander and Kovács, András
                      and Kibkalo, Lidia and Kelemen, Peter B.},
      title        = {{D}uctile deformation during carbonation of serpentinized
                      peridotite},
      journal      = {Nature Communications},
      volume       = {13},
      number       = {1},
      issn         = {2041-1723},
      address      = {[London]},
      publisher    = {Nature Publishing Group UK},
      reportid     = {FZJ-2022-02718},
      pages        = {3478},
      year         = {2022},
      abstract     = {Carbonated serpentinites (listvenites) in the Samail
                      Ophiolite, Oman, record mineralization of 1–2 Gt of CO2,
                      but the mechanisms providing permeability for continued
                      reactive fluid flow are unclear. Based on samples of the
                      Oman Drilling Project, here we show that listvenites with a
                      penetrative foliation have abundant microstructures
                      indicating that the carbonation reaction occurred during
                      deformation. Folded magnesite veins mark the onset of
                      carbonation, followed by deformation during carbonate
                      growth. Undeformed magnesite and quartz overgrowths indicate
                      that deformation stopped before the reaction was completed.
                      We propose deformation by dilatant granular flow and
                      dissolution-precipitation assisted the reaction, while
                      deformation in turn was localized in the weak reacting mass.
                      Lithostatic pore pressures promoted this process, creating
                      dilatant porosity for CO2 transport and solid volume
                      increase. This feedback mechanism may be common in
                      serpentinite-bearing fault zones and the mantle wedge
                      overlying subduction zones, allowing massive carbonation of
                      mantle rocks.},
      cin          = {ER-C-1},
      ddc          = {500},
      cid          = {I:(DE-Juel1)ER-C-1-20170209},
      pnm          = {5351 - Platform for Correlative, In Situ and Operando
                      Characterization (POF4-535)},
      pid          = {G:(DE-HGF)POF4-5351},
      typ          = {PUB:(DE-HGF)16},
      pubmed       = {35710547},
      UT           = {WOS:000812995300021},
      doi          = {10.1038/s41467-022-31049-1},
      url          = {https://juser.fz-juelich.de/record/908609},
}