Project Details
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Viscous relaxation of crust of the Sudbury impact structure, Canada

Subject Area Palaeontology
Term from 2015 to 2021
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 285706348
 
Final Report Year 2021

Final Report Abstract

Based chiefly on structural field evidence from the Sudbury impact structure, Canada, the mechanism of long-term crustal relaxation was addressed by examining mineral fabrics, slip on post-cratering faults, impact melt rock dikes and sulphide veins in target rocks underlying the Sudbury Igneous Complex, Canada. Collectively, the results point to formation of these structures on time scales of tens of thousands of years and kinematically associated with longterm crater modification consistent with relaxation of crust below the impact structure. Significant progress was also achieved in terms of better understanding the chemical evolution and emplacement of Cu-Ni-PGE-rich sulphides in crater floor fractures, known as Offset Dikes at Sudbury. Complemented by a geochemical and geophysical analysis of equivalent impact melt rock dikes of the Vredefort impact structure, South Africa, crustal relaxation occurred kinematically as a direct consequence of dynamic collapse of a transient cavity, however at significantly lower strain rates than occurring during cratering. The results of the project challenge a long-standing paradigm in impact tectonics, in which deformation of target rock is exclusively caused by impact and cratering, both operating on time scales of seconds and minutes, respectively.

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