supported by the National Natural Science Foundation of China(Nos.40972042,40772041,42072030);the Open Research Program of the Key Laboratory of Continental Dynamics,Northwest University
High-temperature magma generation process and granulite-facies metamorphism can provide important information about mantle-crustal interaction and tectonic evolution. The strongly peralu- minous monzonite pluton, the ...
supported by the National Natural Science Foundation of China(Nos.40972042 and 41172069);Hong Kong RGC(No.HKU704312P);the Fundamental Research Funds for the Central Universities of of Ministry of Education,China
The metamorphosed Early Paleoproterozoic granitoids in the Quanji massif, Northwest- ern China provide constraints for relationship between the Tarim Craton and North China Craton. Among granitoids batholiths, rocks o...
supported by the National Natural Science Foundation of China(Nos.40972042,40772041,91014002);the Research Grant Council of Hong Kong RGC(No.HKU705311P)
The Quanji (全吉) Massif is located in the Northwest China, which is interpreted as a micro-continent that is composed of metamorphic basement and stable cover strata. There are some controversies of genetic relatio...