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Ca-rich majorite derived from high-temperature melt and thermally stressed hornblende in shock veins of crustal rocks from the Ries impact crater (Germany)

VolcanologyEngineeringCa-rich MajoriteGeologyHigh-temperature MeltCrustal MeltingGeochemistryHigh Temperature GeochemistryPetrologyIgneous PetrologyEarth ScienceShock VeinsMeteorite ImpactTectonics