• Corpus ID: 56120310

Intra-Conference Field Trip MAY 18 to 20 , 2018 Natural Park of La Garrotxa volcanic field : magmatic vs phreatomagmatic activity . The role of the basement to control the eruptive dynamics

@inproceedings{Mart2018IntraConferenceFT,
  title={Intra-Conference Field Trip MAY 18 to 20 , 2018 Natural Park of La Garrotxa volcanic field : magmatic vs phreatomagmatic activity . The role of the basement to control the eruptive dynamics},
  author={Joan Mart{\'i} and Xavier Bol{\'o}s and Llorenç Planagum{\`a}},
  year={2018}
}

References

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Geological Setting of La Garrotxa Volcanic Field

Situated in the northeast of the Iberian Peninsula, La Garrotxa Volcanic Field is part of the Catalan Volcanic Zone and one of the provinces of the Neogene-Quaternary alkaline volcanism associated

Geophysical exploration on the subsurface geology of La Garrotxa monogenetic volcanic field (NE Iberian Peninsula)

We applied self-potential (SP) and electrical resistivity tomography (ERT) to the exploration of the uppermost part of the substrate geology and shallow structure of La Garrotxa monogenetic volcanic

Structural control of monogenetic volcanism in the Garrotxa volcanic field (Northeastern Spain) from gravity and self-potential measurements

We report new geophysical observations on the distribution of subsurface structures associated with monogenetic volcanism in the Garrotxa volcanic field (Northern Spain). As part of the Catalan