Earth's anomalous middle-age magmatism driven by plate slowdown

The mid-Proterozoic or boring billion exhibited extremely stable environmental conditions, with little change in atmospheric oxygen levels, and mildly oxygenated shallow oceans. A limited number of passive margins with extremely long lifespans are observed from this time, suggesting that subdued tectonic activity-a plate slowdown-was the underlying reason for the environmental stability. However, the Proterozoic also has a unique magmatic and metamorphic record; massif-type anorthosites and anorogenic Rapakivi granites are largely confined to this period and the temperature/pressure (thermobaric ratio) of granulite facies metamorphism peaked at over 1500 degrees C/GPa during the Mesoproterozoic. Here, we develop a method of calculating plate velocities from the passive margin record, benchmarked against Phanerozoic tectonic velocities. We then extend this approach to geological observations from the Proterozoic, and provide the first quantitative constraints on Proterozoic plate velocities that substantiate the postulated slowdown. Using mantle evolution models, we calculate the consequences of this slowdown for mantle temperatures, magmatic regimes and metamorphic conditions in the crust. We show that higher mantle temperatures in the Proterozoic would have resulted in a larger proportion of intrusive magmatism, with mantle-derived melts emplaced at the Moho or into the lower crust, enabling the production of anorthosites and Rapakivi granites, and giving rise to extreme thermobaric ratios of crustal metamorphism when plate velocities were slowest.

Automated summary

The mid-Proterozoic period, known as the boring billion, was characterized by stable environmental conditions and limited tectonic activity. This period also witnessed unique magmatic and metamorphic events, such as the formation of anorthosites and Rapakivi granites. Researchers have developed a method to calculate plate velocities during this time and have found evidence supporting the hypothesis of a plate slowdown. The higher mantle temperatures during the Proterozoic resulted in increased intrusive magmatism and extreme thermobaric ratios of crustal metamorphism.