Publication 184

3D multi-observable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle. III: Thermochemical Tomography in the Western-Central US

Afonso, J.C., N. Rawlinson, Y. Yang, D.L. Schutt, A.G. Jones, J. Fullea, and W.L. Griffin


We apply a novel 3D multi-observable probabilistic tomography method that we have recently developed and benchmarked [Afonso et al. 2013a;b], to directly image the thermochemical structure of the Colorado Plateau and surrounding areas by jointly inverting P-wave and S-wave teleseismic arrival times, Rayleigh wave dispersion data, Bouguer anomalies, satellite-derived gravity gradients, geoid height, absolute (local and dynamic) elevation, and surface heat flow data. The temperature and compositional structures recovered by our inversion reveal a high level of correlation between recent basaltic magmatism and zones of high temperature and low Mg# (i.e. refertilized mantle) in the lithosphere, consistent with independent geochemical data. However, the lithospheric mantle is overall characterised by a highly heterogeneous thermochemical structure, with only some features correlating well with either Proterozoic and/or Cenozoic crustal structures. This suggests that most of the present-day deep lithospheric architecture re- flects the superposition of numerous geodynamic events of different scale and nature to those that created major crustal structures. This is consistent with the complex lithosphere-asthenosphere system that we image, which exhibits a variety of multi-scale feedback mechanisms (e.g. small-scale convection, magmatic intrusion, delamination, etc) driving surface processes. Our results also suggest that most of the present-day elevation in the Colorado Plateau and surrounding regions is the result of thermochemical buoyancy sources within the lithosphere, with dynamic effects (from sublithospheric mantle flow) contributing only locally up to ∼15-35%.


Journal of Geophysical Research - Solid Earth, 121, 7337-7370, doi:10.1002/2016JB013049. [PDF]; Note: Editors' Highlight

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Alan G Jones / 17 March 2017 / alan.jones.geophysics -at-