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《Geochimica》 1985-01
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USE OF REE IN APATITES TO DISTINGUISH THE PETROGENO-MINERALIZATION SERIES OF GRANITIC ROCKS

Zhang Shaoli Wang Liankui Zhu Weifang Yang Wenjin (Institute of Geochemistry, Academia Sinica)  
REE investigations of apatites from two series of granitic rocks, including more than ten types of rock and several tens of rock masses in eight south China's provinces permit us to have come to some new understanding and hence the following conclusions have been drawn.Apatites from different series of granitic rocks show significant differences in REE distribution, probably due to different source materials. Therefore, REE distribution characteristics can be used to distinguish source-different granitic rocks. The apatites in granites of the Nanling series (derived from the shallow crust) have a lower content of ∑REE (4571 ppm on average). In the apatites Y is the highest of the REE group. ∑Y is rich relative to ∑ Ce, thus giving rise to relatively low ∑ Ce/∑Y ratio (0.68 on average) Eu shows strong depletion, and 6 Eu is extremely low (0.135 on average). The REE distribution patterns are represented by the "V"-shaped symmetric curves. The apatites in granites o'f the Changjiang (Yangtze) series are relatively high in ?REE (8571.3 ppm on average) Ce is the highest of the REE group. ∑Ce is rich relative to∑Y and the ∑Ce/∑Y is relatively high (7.15 on average) in the apatites from the Ya-ngtze series. The chondrite-normalized REE distribution patterns are characterized by the rightward-inclined curves.
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