The flexural rigidity of Fennoscandia: reflection of the tectonothermal age of the lithospheric mantle

Estimates of effective elastic thickness (Te), a measure of the strength of the plate, have shown that older and cool cratonic regions are characteris ed by a stronger lithosphere (higher Te values) than areas which have been tectonically reworked. We use geophysical data and information from xenolit hs in volcanic rocks from Fennoscandia and show that the strength of the li thosphere reflects the tectonothermal age of the lithospheric mantle. Fenno scandia is made up of the Baltic shield (1.9-3.0 Ga) and the Caledonian Oro gen of Norway and northern Sweden (400-500 Ma). The shield is characterised by an old, thick and cold lithosphere in contrast to the Caledonides where the lithosphere is hotter and thinner. Our geophysical analysis results sh ow a regional variation in elastic plate thickness from 8 km to 70 km, or e quivalently, a flexural rigidity between 0.4X10(22) and 3X10(24) Nm. These results suggest that the lithosphere is strongest In the relatively stable Archaean Province, weaker in the regions characterised by Proterozoic crust al formation, and lowest in the tectonically reworked and deformed Caledoni an belt. Within the study area, there is a direct correlation between litho sphere strength, the age of the last major tectonothermal event registered in the crust and lithospheric mantle composition. These broad correlations reflect thinner and more fertile lithosphere, and higher geothermal gradien ts, beneath regions of progressively younger crust. served.