Cargando…
Marine Geophysical Investigation of the Chain Fracture Zone in the Equatorial Atlantic From the PI‐LAB Experiment
The Chain Fracture Zone is a 300‐km‐long transform fault that offsets the Mid‐Atlantic Ridge. We analyzed new multibeam bathymetry, backscatter, gravity, and magnetic data with 100% multibeam bathymetric data over the active transform valley and adjacent spreading segments as part of the Passive Ima...
Autores principales: | Harmon, Nicholas, Rychert, Catherine, Agius, Matthew, Tharimena, Saikiran, Le Bas, Tim, Kendall, J. Michael, Constable, Steven |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
John Wiley and Sons Inc.
2018
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6472653/ https://www.ncbi.nlm.nih.gov/pubmed/31007998 http://dx.doi.org/10.1029/2018JB015982 |
Ejemplares similares
-
Sediment Characterization at the Equatorial Mid‐Atlantic Ridge From P‐to‐S Teleseismic Phase Conversions Recorded on the PI‐LAB Experiment
por: Agius, M. R., et al.
Publicado: (2018) -
Sediment structure at the equatorial mid-atlantic ridge constrained by seafloor admittance using data from the PI-LAB experiment
por: Saikia, Utpal, et al.
Publicado: (2020) -
Scattered wave imaging of the oceanic plate in Cascadia
por: Rychert, Catherine A., et al.
Publicado: (2018) -
Seismic Crustal Structure and Morphotectonic Features Associated With the Chain Fracture Zone and Their Role in the Evolution of the Equatorial Atlantic Region
por: Marjanović, Milena, et al.
Publicado: (2020) -
Distribution and activity of diazotrophs in the Eastern Equatorial Atlantic
por: Foster, Rachel A, et al.
Publicado: (2009)