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The Early Cretaceous granitic complex in Highland 1248 of Daxing’anling successively consists of intruded granodiorite,monzonite granite and syenite granite. Through test analysis on the major,trace and rare earth elements of the intrusive complex,this study focuses on the source characteristics and tectonic environment of the original magma of intrusive complex. The results show that the intrusive rocks in Highland 1248 are meta-aluminous-peraluminous rocks in calc-alkaline series with homologous characteristics in δEu negative anomalies; the complex is enriched in LILE( Rb,Cs and K) and depleted in HFSE( lanthanide,Sc,Y,U,Nb and Ta),displaying the geochemical characteristics of I-type granites in active continental-margin subduction zones. The complex also has the characteristics of granites after the collision of plate with rich aluminum and high potassium,but significantly depleted Nb,Ta,Ti,P and other elements,i. e. in the orogenic evolutionary stage. The zircon U-Pb SHRIMP isotopic apparent age of the complex in Highland 1248 is 140. 0--141. 0Ma,and the formation time is in Early Cretaceous.
The Early Cretaceous granitic complex in Highland 1248 of Daxing’anling comprises consists of intruded granodiorite, monzonite granite and syenite granite. Through test analysis on the major, trace and rare earth elements of the intrusive complex, this study focuses on the source characteristics and tectonic environment of the original magma of intrusive complex. The results show that the intrusive rocks in Highland 1248 are meta-aluminous-peraluminous rocks in calc-alkaline series with homologous characteristics in δEu negative anomalies; the complex is enriched in LILE (Rb, Cs and K) and depleted in HFSE (lanthanide, Sc, Y, U, Nb and Ta), displaying the geochemical characteristics of I-type granites in active continental-margin subduction zones. The complex also has the characteristics of granites after the collision of plate with rich aluminum and high potassium, but significantly depleted Nb, Ta, Ti, P and other elements, ie in the orogenic evolutionary stage. The zircon U-Pb SHRIMP isoto pic apparent age of the complex in Highland 1248 is 140. 0--141. 0Ma, and the formation time is in Early Cretaceous.