Glisovic P, Forte A.M., 2019. Two deep mantle sources for Paleocene doming and volcanism in the North Atlantic. Proceedings of the National Academy of Sciences, doi: 10.1073/pnas.1816188116.
Links to the following data:
- A convection prediction of mantle heterogeneity below the North Atlantic at 55 Ma (Fig. 1).
- A prediction of mantle melt production (Fig. 2).
- Particle trajectories predicted with time-dependent flow reconstructions (Fig. 3).
- Paleogene predictions of dynamic surface topography (Fig. 4).
- Cross-correlation coefficients (SI Appendix, Fig. S1).
- Convection reconstructions of mantle heterogeneity below the North Atlantic over the Cenozoic (SI Appendix, Fig S3).
- Mantle flow predictions (SI Appendix, Fig. S4).
- Cluster analysis of the vertical flow field predicted with three tomography models (SI Appendix, Fig. S5).
- Reference temperature profiles that satisfy a half-space cooling model for different lithospheric ages (SI Appendix, Fig. S6).
- The depth variation of total melt areas (SI Appendix, Fig. S7).
- Mantle flow lines under the North Atlantic (SI Appendix, Fig. S8).
- The total volume of mantle melting for tomography-based convection models over the last 70 Myr (SI Appendix, Fig. S9).
- Paleogene predictions of dynamic surface topography (SI Appendix, Fig. S10).
- The evolution of theoretical plumes and associated surface dynamic topography in the North Atlantic (SI Appendix, Fig. S11).
- Geotherm profiles employed in the mantle convection simulations (SI Appendix, Fig. S12).
- A comparison between initial and predicted models of mantle density heterogeneity (SI Appendix, Fig. S13).
- Particle flow lines predicted by a model of tomography-based present-day mantle flow (SI Appendix, Fig. S14).
Please contact Petar Glisovic at pglisovic [at] gmail.com for any additional request.