Synchronous peak Barrovian metamorphism driven by syn-orogenic magmatism and fluid flow in southern Connecticut , USA

@inproceedings{Lancaster2008SynchronousPB,
  title={Synchronous peak Barrovian metamorphism driven by syn-orogenic magmatism and fluid flow in southern Connecticut , USA},
  author={Paul Lancaster and Ethan F. Baxter and Jay J. Ague and C. M. BREEDING and Tracie L Owens},
  year={2008}
}
Recent work in Barrovian metamorphic terranes has found that rocks experience peak metamorphic temperatures across several grades at similar times. This result is inconsistent with most geodynamic models of crustal over-thickening and conductive heating, wherein rocks which reach different metamorphic grades generally reach peak temperatures at different… CONTINUE READING