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Mafic/ultramafic rocks derived from high siliceous(high-Si)high magnesium(high-Mg)mantle melts are an important feature observed during early Precambrian.They provide much important geological and petrological
Mafic / ultramafic rocks derived from high siliceous (high-Si) high magnesium (high-Mg) mantle melts are an important feature observed during early Precambrian. They provide much important geological and petrological