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...

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Detalles Bibliográficos
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:
Research Articles
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

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6472653/
https://www.ncbi.nlm.nih.gov/pubmed/31007998
http://dx.doi.org/10.1029/2018JB015982

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