Petrogenesis of the Middle Triassic Erenhot granitoid batholith in central Inner Mongolia (northern China) with tectonic implication for the Triassic Mo mineralization in the eastern Central Asian Orogenic Belt
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Pre One:Juvenile crustal recycling in an accretionary orogen: Insights from contrasting Early Permian granites from central Inner Mongolia, North China
Next One:Early Cretaceous gabbro-granite complex from central Inner Mongolia: Insights into initial rifting and crust-mantle interaction in the northern China-Mongolia basin-range tract
