Cargando…
Sediment structure at the equatorial mid-atlantic ridge constrained by seafloor admittance using data from the PI-LAB experiment
Well-constrained marine sediment characteristics (sediment thickness and shear wave velocity) are important not only for the study of climate over geologic times scales but also for correcting and accounting for its presence in seismic data used to investigate deeper structures. We use data from the...
Autores principales: | Saikia, Utpal, Rychert, Catherine, Harmon, Nicholas, Kendall, J. M. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer Netherlands
2020
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7357728/ https://www.ncbi.nlm.nih.gov/pubmed/32684641 http://dx.doi.org/10.1007/s11001-020-09402-0 |
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) -
Marine Geophysical Investigation of the Chain Fracture Zone in the Equatorial Atlantic From the PI‐LAB Experiment
por: Harmon, Nicholas, et al.
Publicado: (2018) -
Anomalous K-Pg–aged seafloor attributed to impact-induced mid-ocean ridge magmatism
por: Byrnes, Joseph S., et al.
Publicado: (2018) -
The Role of Oceanic Transform Faults in Seafloor Spreading: A Global Perspective From Seismic Anisotropy
por: Eakin, Caroline M., et al.
Publicado: (2018) -
Seafloor hydrothermal activity along mid-ocean ridge with strong melt supply: study from segment 27, southwest Indian ridge
por: Yue, Xihe, et al.
Publicado: (2019)