Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems

J. E. Johnson, C. Hans Nelson, C. Goldfinger

Open source

DOI: 10.4401/ag-3452
Published: 06
Container: Annals of Geophysics
Publisher: Not recorded
Open access: yes

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Cite this work

BibTeX

@article{allodium:10.4401/ag-3452,
  title = {Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems},
  author = {J. E. Johnson and C. Hans Nelson and C. Goldfinger},
  year = {2003},
  journal = {Annals of Geophysics},
  doi = {10.4401/ag-3452},
  url = {https://doi.org/10.4401/ag-3452}
}

RIS

TY  - JOUR
TI  - Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems
AU  - J. E. Johnson
AU  - C. Hans Nelson
AU  - C. Goldfinger
PY  - 2003
JO  - Annals of Geophysics
DO  - 10.4401/ag-3452
UR  - https://doi.org/10.4401/ag-3452
ER  -

APA

Johnson, J. E., Nelson, C. H., & Goldfinger, C. (2003). Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems. Annals of Geophysics. https://doi.org/10.4401/ag-3452

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doaj · retrieved 2026-09-25T02:29:16.552Z