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TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day

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Page 1: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day
Page 2: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day
Page 3: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day
Page 4: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day
Page 5: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day
Page 6: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day
Page 7: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day
Page 8: TU Clausthal · Archaean crust formation by crystal-liquid frac- tionation of primitive mantle material and dominantly intracrustal fractionation in the Phanerozoic led to the present-day

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