Magnetic anomaly identifications form the primary data set from which the age of the oceanic lithosphere can be determined, a critical component of reconstructing the seafloor spreading history of ocean basins. This data is now available as part of an open source, community-driven online repository that contains quality-checked magnetic anomaly picks, organised by ocean basin and publication source.
Nature Communications – Rift migration explains continental margin assymetry and crustal hyper-extension
Brune, S., Heine, C., Pérez-Gussinyé, M., & Sobolev, S. V. (2014). Rift migration explains continental margin asymmetry and crustal hyper-extension. Nature communications, 5. doi: 10.1038/ncomms5014. Rift migration explains continental margin asymmetry and crustal hyper-extension Download supplementary information – pdf
