@misc{CescaStichGrigolietal.2022,
  author    = {Cesca, Simone and Stich, Daniel and Grigoli, Francesco and Vuan, Alessandro and L{\´o}pez-Comino, Jos{\´e} {\´A}ngel and Niemz, Peter and Blanch, Estefan{\´i}a and Dahm, Torsten and Ellsworth, William L.},
  title     = {Reply to: Multiple induced seismicity mechanisms at Castor underground gas storage illustrate the need for thorough monitoring},
  series = {Nature communications},
  volume    = {13},
  journal   = {Nature communications},
  number    = {1},
  publisher = {Nature Research},
  address   = {Berlin},
  issn      = {2041-1723},
  doi       = {10.1038/s41467-022-30904-5},
  pages     = {4},
  year      = {2022},
  language  = {en}
}
@article{CescaSuganRudzinskietal.2022,
  author    = {Cesca, Simone and Sugan, Monica and Rudzinski, Lukasz and Vajedian, Sanaz and Niemz, Peter and Plank, Simon and Petersen, Gesa and Deng, Zhiguo and Rivalta, Eleonora and Vuan, Alessandro and Linares, Milton Percy Plasencia and Heimann, Sebastian and Dahm, Torsten},
  title     = {Massive earthquake swarm driven by magmatic intrusion at the Bransfield Strait, Antarctica},
  series = {Communications earth and environment},
  volume    = {3},
  journal   = {Communications earth and environment},
  number    = {1},
  publisher = {Springer Nature},
  address   = {London},
  issn      = {2662-4435},
  doi       = {10.1038/s43247-022-00418-5},
  pages     = {11},
  year      = {2022},
  abstract  = {An earthquake swarm affected the Bransfield Strait, Antarctica, a unique rift basin in transition from intra-arc rifting to ocean spreading. The swarm, counting similar to 85,000 volcano-tectonic earthquakes since August 2020, is located close to the Orca submarine volcano, previously considered inactive. Simultaneously, geodetic data reported up to similar to 11 cm north-westward displacement over King George Island. We use a broad variety of geophysical data and methods to reveal the complex migration of seismicity, accompanying the intrusion of 0.26-0.56 km(3) of magma. Strike-slip earthquakes mark the intrusion at depth, while shallower normal faulting the similar to 20 km long lateral growth of a dike. Seismicity abruptly decreased after a Mw 6.0 earthquake, suggesting the magmatic dike lost pressure with the slipping of a large fault. A seafloor eruption is likely, but not confirmed by sea surface temperature anomalies. The unrest documents episodic magmatic intrusion in the Bransfield Strait, providing unique insights into active continental rifting.},
  language  = {en}
}