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U–Th systematics of dispersed young volcanoes in NE China: Asthenosphere upwelling caused by piling up and upward thickening of stagnant Pacific slab

GeophysicsVolcanologyEngineeringVolcanismDispersed Young VolcanoesSubduction ZoneNe ChinaGeologyVolcanic ProcessCrust-mantle InteractionU–th SystematicsEarth ScienceTectonics