ULTRAHIGH-PRESSURE METAMORPHISM—PAST RESULTS AND FUTURE PROSPECTS
Circumpacific-type blueschists and eclogites worldwide form in penetratively deformed allochthonous slabs and nappes verging seaward, requiring underflow of oceanic basement (30-50 km) during metamorphism. Neoblastic coesite and microdiamond inclusions found in tough, rigid container minerals demonstrate that Alpine-type continental collision involves partial recovery of rocks far more deeply subducted (100-130 km) than previously imagined. Even more surprising, garnet lherzolites from the central Alps, east-central China, and western Norway display mineral intergrowths and exsolution lamellae reflecting the initial presence of majoritic garnet, requiring even greater depths of origin of host peridotites (>300 km). Nano-minerals hold yet another key to deciphering the actual depths of subduction and mantle return flow. The duration of storage at great depth and exhumation rates are current problems. Fluid-rock and lithosphere-asthenosphere interactions have recycled volatiles to the deep Earth through both hydrous and nominally anhydrous phases. Mantle petrochemistry and dynamics (plumes + plates) control the evolving architecture of the crust and the biosphere dependent on it, hence synergies between advanced technologies and condensed ultrahigh-pressure materials will lead to a fuller understanding of the Earth in time and space.