Cahracteristics of progressive ductile deformation and remnant igneous fabrics indicate that the foliated diorites in the middle sector of the Jiangshao fractur
On the basis of the previous quantitative modeling of trace element behavior in magmatic pro-cesses such as fractional crystallization ,batch melting and magma
The comprehensive results of whole-rock Sm-Nd and Rb-Sr and zircon Pb-Pb dating suggest that the Qinling Group in the Qinling orogenic belt, northwestern Henan