Fig. S12: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Fig. S13: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Fig. S11: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Figs S26 and S27: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Fig. S8: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Fig. S14: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Fig. S19: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Late Cretaceous to Paleogene tectonometamorphic evolution of the Shuswap Metamorphic Complex, British Columbia
Fig. S10: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
Table S2: Prolonged high-temperature Caledonian metamorphism in the southern part of the Northern Highlands terrane, Scotland, indicated by integrated monazite and xenotime laser ablation split-stream petrochronology and thermometry
