Project Details
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Linking the deep structures of the cratons of Africa and South America by integrated geophysical modelling

Subject Area Geophysics
Term from 2017 to 2022
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 336717379
 
Final Report Year 2022

Final Report Abstract

In our project, we studied the cratons of South America and Africa by (i) satellite gravity inversion and (ii) thermo-compositional modelling. Our novel satellite gravity inversion uses seismic tomography in form of a regionalization map, in turn based on cluster analysis, as constraint and allows hereby to laterally vary the density contrast in the inversion. While inverting for a single density contrast is a simplification, it provides first insights into the lithospheric architecture, which is in focus of the dedicated thermo-compositional modelling. Here, seismic tomography and seismic depth estimates are used as constraint as before, but additional sources in the lithosphere are addressed. The results show that the crustal and upper mantle of the cratons of South America and Africa is more complex than previously thought and that their tectonic evolution is less homogeneous. This is also illustrated by studying the passive margin architecture and opening of the South Atlantic as this allows to enhance the structural similarities between the cratons. The break-up of Central Gondwana did affect the cratons, but structural similarities still exists between the two sides of the Atlantic. The results of the project hold the promise for an improve general understanding of the evolution of cratons, when applied on a global scale as done already for the satellite gravity gradient inversion.

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