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《Earth Science-Journal of China University of Geosciences》 1993-01
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COMPOSITIONAL POLARITY AND GENESIS OF ARC GRANITOIDS IN DANFENG-XIXIA AREA, NORTH QINLING OROGENIC BELT

Luo Tingchuan Zhang Hongfei Zhang Benrcn (China University of Geosciences, Wuhan 430074)  
The Early Paleozoic granitoids in the Danfeng-Xixia area have geochemical characteristics of arc granitoids, and were products of the northeastern subduction of the paleo-Qin-ling ocean along the Shangdan main suture. At similar SiO2 levels, granitoids of the same type, in form of either stock or batholith, all show compositional trans-arc polarities, i. e. increase towards continent in K,O. K2O + Na2O, K2O/Na2O, ΣREE, La, Rb, Th, Zr, δ18O and 87Sr/86Sr. The polarity can be attributed to the corresponding increase of crustal components in the magma source towards the same direction.
【Fund】: 国家自然科学基金;; 地质行业科学发展基金(项目号48970171)
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