Zircon U–Pb ages, Hf–O isotopes and trace elements of Mesozoic high Sr/Y porphyries from Ningzhen, eastern China: Constraints on their petrogenesis, tectonic implications and Cu mineralization

Lithos ◽  
2014 ◽  
Vol 200-201 ◽  
pp. 299-316 ◽  
Author(s):  
Fangyue Wang ◽  
Sheng-Ao Liu ◽  
Shuguang Li ◽  
Shamim Akhtar ◽  
Yongsheng He
2018 ◽  
Vol 11 (3) ◽  
pp. 195-207 ◽  
Author(s):  
Long Sun ◽  
Manus Carey ◽  
Lei Yang ◽  
Li-Ding Chen ◽  
Shou-Juan Li ◽  
...  

2000 ◽  
Vol 64 (5) ◽  
pp. 867-877 ◽  
Author(s):  
R. C. Wang ◽  
G. T. Zhao ◽  
J. J. Lu ◽  
X. M. Chen ◽  
S. J. Xu ◽  
...  

AbstractZircon commonly occurs as one of important accessory HFSE-bearing minerals in A-type granite. A detailed electron microprobe study was carried out on zircon from the Laoshan complex, Eastern China, which is composed of I- and A-type granites. Zircon from the I-type rocks is relatively poor in trace elements (HfO2<2 wt.%, UO2, ThO2 and Y2O3 <1 wt.%), but that from the A-type rocks is richer in Hf, U, Th and Y. Hafnian zircon with a HfO2 content of up to 12.37 wt.% was found in the arfvedsonite granite, which is considered the most evolved facies in the A-type suite. Enrichment in Hf is generally observed at the rims of zircon crystals relative to the cores. The Hf enrichment in zircon, and the association of exotic REE- and HFSE-bearing minerals are linked to hydrothermal activity, suggesting that during the last stage of crystallization of the A-type magma, fluids enriched in REE, HFSE, F−, CO32− and PO43− were released.


2019 ◽  
Vol 30 (6) ◽  
pp. 1230-1242 ◽  
Author(s):  
Zhaojun Song ◽  
Huimin Liu ◽  
Fanxue Meng ◽  
Xingyu Yuan ◽  
Qiao Feng ◽  
...  

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