Supported by National Natural Science Foundation of China (Grant Nos. 40772042, 90714010, 40873043 and 40821061);the Ministry of Education of China (Grant Nos. IRT0441, B07039 and NCET-06-0659);the Opening Foundation of the State Key Laboratory of Continental Dynamics, Northwest University
Here we report an integrated study of zircon U-Pb age and Hf isotope composition for a gneiss sample from the Kongling terrain in the Yangtze Craton. CL imaging reveals that most zircons are magmatic, and a few of the...
Supported by the National Basic Research Program of China (Grant No. 2009CB825000);National Natural Science Foundation of China (Grant Nos. 40873043, 40821061, 90714010 and 40772042);Ministry of Education of China (Grant Nos. IRT0441, B07039 and NCET-06-0659);Foundation of the State Key Laboratory of Continental Dynamics, Northwest University
The foramtion and evolution of collisional orogen is a prominent feature along convergent plate margins, and is generally a complex process. This article presents an integrated study of zircon genesis, U-Pb age and Lu...
Supported by National Natural Science Foundation of China (Grant Nos. 40772042, 90714010 and 40521001);the Ministry of Education of China (Grant Nos. IRT0441, B07039 and NCET-06-0659);Foundation of the State Key Laboratory of Continental Dynamics, Northwest University
Mafic dyke is a sign of regional extension, and thus has important tectonic significance. A great amount of mafic dykes occur in the Kongling terrain of the Yangtze Craton, which have great bearing on the early evolut...
Supported by National Natural Science Foundation of China (Grant Nos. 90714002 and 40772042) ;National Basic Research Program of China (Grant No. 2006CB403502)
Zircon U-Pb age and Hf isotope, and major and trace element compositions were reported for granite at Quanyishang, which intruded into the Kongling complex in Yichang, Hubei Province. The results show that the Quanyis...