Characteristics of mantle source for Jining Cenozoic basalts from southern Inner Mongolia:evidence from element and Sr-Nd-Pb isotopic geochemistry.Acta Petrologica;

All these features indicate consistently that the ore-bearing magma was derived from an enriched lithospheric mantle source which had been metasomatized by the subducted sedimentary melt,and that the magma originated from a source with low extent of partial melting (about 10%) at a shallow depth of the spinel lherzolite facies.

Mantle source characteristics of magmatic carbonatites from the Himalayan Collision Zone in western Sichuan,SW China:Evidence of Pb-Sr-Nd isotopes.;