Seismicity properties of the Chain Transform Fault inferred using data from the PI-LAB experiment

Autor: Leptokaropoulos, K, Rychert, CA, Harmon, N, Kendall, JM

Oceanic transform faults are intriguing in that they do not produce earthquakes as large as might be expected given their dimensions. We use 1-year of local seismicity (370 events above MC = 2.3) recorded on an array of ocean bottom seismometers (OBS

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8dc1dbb2b000559c4c541e2e31e131a5
https://doi.org/10.1002/essoar.10511418.1

Broad fault zones enable deep fluid transport and limit earthquake magnitudes.

Autor: Leptokaropoulos K; Ocean and Earth Science, University of Southampton, Southampton, UK. K.Leptokaropoulos@soton.ac.uk.; The MathWorks, Cambridge, UK. K.Leptokaropoulos@soton.ac.uk., Rychert CA; Ocean and Earth Science, University of Southampton, Southampton, UK. catherine.rychert@whoi.edu.; Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, USA. catherine.rychert@whoi.edu., Harmon N; Ocean and Earth Science, University of Southampton, Southampton, UK.; Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, USA., Schlaphorst D; Instituto Dom Luiz (IDL), Faculdade de Ciências, Universidade de Lisboa, Lisbon, Portugal., Grevemeyer I; GEOMAR Helmholtz Centre of Ocean Research Kiel, RD4-Marine Geodynamics, Kiel, Germany., Kendall JM; School of Earth Sciences, University of Oxford, Oxford, UK., Singh SC; Université de Paris, Institut de Physique du Globe de Paris, CNRS, Paris, France.

Publikováno v: Nature communications [Nat Commun] 2023 Sep 16; Vol. 14 (1), pp. 5748. Date of Electronic Publication: 2023 Sep 16.

Subduction history of the Caribbean from upper-mantle seismic imaging and plate reconstruction.

Autor: Braszus B; Geophysical Institute (GPI), Karlsruhe Institute of Technology, Karlsruhe, Germany. benedikt.braszus@kit.edu., Goes S; Department of Earth Science and Engineering, Imperial College London, London, UK. s.goes@imperial.ac.uk., Allen R; Department of Earth Science and Engineering, Imperial College London, London, UK., Rietbrock A; Geophysical Institute (GPI), Karlsruhe Institute of Technology, Karlsruhe, Germany., Collier J; Department of Earth Science and Engineering, Imperial College London, London, UK., Harmon N; National Oceanography Centre, University of Southampton, Southampton, UK., Henstock T; National Oceanography Centre, University of Southampton, Southampton, UK., Hicks S; Department of Earth Science and Engineering, Imperial College London, London, UK., Rychert CA; National Oceanography Centre, University of Southampton, Southampton, UK., Maunder B; Department of Earth Science and Engineering, Imperial College London, London, UK., van Hunen J; Department of Earth Sciences, Durham University, Durham, UK., Bie L; Geophysical Institute (GPI), Karlsruhe Institute of Technology, Karlsruhe, Germany., Blundy J; School of Earth Sciences, University of Bristol, Bristol, UK., Cooper G; School of Earth Sciences, University of Bristol, Bristol, UK., Davy R; Department of Earth Science and Engineering, Imperial College London, London, UK., Kendall JM; Department of Earth Sciences, University of Oxford, Oxford, UK., Macpherson C; Department of Earth Sciences, Durham University, Durham, UK., Wilkinson J; Department of Earth Science and Engineering, Imperial College London, London, UK.; Natural History Museum, London, UK., Wilson M; School of Earth and Environment, University of Leeds, Leeds, UK.

Publikováno v: Nature communications [Nat Commun] 2021 Jul 09; Vol. 12 (1), pp. 4211. Date of Electronic Publication: 2021 Jul 09.

A thin mantle transition zone beneath the equatorial Mid-Atlantic Ridge.

Autor: Agius MR; Ocean and Earth Science, University of Southampton, Southampton, UK. matthew.agius@soton.ac.uk.; Dipartimento di Scienze, Università degli studi Roma Tre, Rome, Italy. matthew.agius@soton.ac.uk., Rychert CA; Ocean and Earth Science, University of Southampton, Southampton, UK., Harmon N; Ocean and Earth Science, University of Southampton, Southampton, UK., Tharimena S; Ocean and Earth Science, University of Southampton, Southampton, UK.; Institute for Meteorology and Geophysics, University of Vienna, Vienna, Austria., Kendall JM; Department of Earth Sciences, University of Oxford, Oxford, UK.

Publikováno v: Nature [Nature] 2021 Jan; Vol. 589 (7843), pp. 562-566. Date of Electronic Publication: 2021 Jan 27.

Variable water input controls evolution of the Lesser Antilles volcanic arc.

Autor: Cooper GF; School of Earth Sciences, University of Bristol, Bristol, UK. CooperG3@cardiff.ac.uk.; School of Earth and Ocean Sciences, Cardiff University, Cardiff, UK. CooperG3@cardiff.ac.uk., Macpherson CG; Department of Earth Sciences, Durham University, Durham, UK., Blundy JD; School of Earth Sciences, University of Bristol, Bristol, UK., Maunder B; Department of Earth Science and Engineering, Imperial College London, London, UK., Allen RW; Department of Earth Science and Engineering, Imperial College London, London, UK., Goes S; Department of Earth Science and Engineering, Imperial College London, London, UK., Collier JS; Department of Earth Science and Engineering, Imperial College London, London, UK., Bie L; Geophysical Institute (GPI), Karlsruhe Institute of Technology, Karlsruhe, Germany., Harmon N; University of Southampton, National Oceanography Centre, Southampton, UK., Hicks SP; Department of Earth Science and Engineering, Imperial College London, London, UK., Iveson AA; Department of Earth Sciences, Durham University, Durham, UK., Prytulak J; Department of Earth Sciences, Durham University, Durham, UK., Rietbrock A; Geophysical Institute (GPI), Karlsruhe Institute of Technology, Karlsruhe, Germany., Rychert CA; University of Southampton, National Oceanography Centre, Southampton, UK., Davidson JP; Department of Earth Sciences, Durham University, Durham, UK.

Publikováno v: Nature [Nature] 2020 Jun; Vol. 582 (7813), pp. 525-529. Date of Electronic Publication: 2020 Jun 24.