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《Mineral Deposits》 2015-01
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Zircon germanium and age constrains on source of Lincang germanium deposit,Yunnan Province

LIU DeLiang;HUANG QiShuai;SHI RenDeng;YUE YaHui;Ding Lin;Key Laboratory of Continental Collision and Plateau Uplift,Institute of Tibetan Plateau Research, Chinese Academy of Sciences;  
The Lincang deposit occurs in the Miocene fault depressions overlying the Lincang batholith in Yunnan Province. It is generally accepted that Ge in the deposit was sourced from the underlying granites. However, the Lincang batholith is a composite one, and has experienced multi-magmatic pulses. It remains unclear which magmatic stage provided germanium to the deposit. This paper reports in-situ LA-ICP-MS Ge and U-Pb isotopic measurements of zircons in granites collected near Xiaojie, Lincang, Mengku and Menghai, which pass southwards through the Lincang batholith. The results achieved show that the timing of the main magmatic stage is between( 215. 6 ± 2. 7)Ma and( 236. 9 ± 3. 7) Ma, and zircons of these granites have low Ge concentrations( 0. 23 × 10- 6~ 4. 21 × 10- 6,0. 53 × 10- 6on average). Inherited zircons with ages between 303 Ma and 2533 Ma also have low Ge concentrations( 0. 34 × 10- 6~ 3. 43 × 10- 6, 1. 18 × 10- 6on average). In contrast, the newly identified zircons 106 Ma and87 Ma in age have high Ge concentrations up to 102 × 10- 6. It is proposed that Ge in the Lincang deposit was likely sourced from late stage magmatic or hydrothermal activities.
【Fund】: 中国科学院知识创新工程重要方向项目(编号:KZCX2-YW-Q04-01)资助
【CateGory Index】: P618.75
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