Using trace elements of magnetite to constrain the origin of the Pingchuan hydrothermal low-Ti magnetite deposit in the Panxi area, SW China

2019 ◽  
Vol 38 (3) ◽  
pp. 376-390
Author(s):  
Yanjun Wang ◽  
Weiguang Zhu ◽  
Hong Zhong ◽  
Zhongjie Bai ◽  
Junhua Yao ◽  
...  
Keyword(s):  
Sw China ◽  

2021 ◽  
Vol 12 (2) ◽  
pp. 605-623 ◽  
Author(s):  
Jun Chen ◽  
Zhi-Long Huang ◽  
Rui-Dong Yang ◽  
Li-Juan Du ◽  
Ming-Yang Liao




2017 ◽  
Vol 76 (7) ◽  
Author(s):  
Jing Liu ◽  
Si-Liang Li ◽  
Jiu-Bin Chen ◽  
Jun Zhong ◽  
Fu-Jun Yue ◽  
...  




2019 ◽  
Vol 113 ◽  
pp. 103067 ◽  
Author(s):  
Yuzhou Zhuo ◽  
Ruizhong Hu ◽  
Jiafei Xiao ◽  
Chenghai Zhao ◽  
Yong Huang ◽  
...  


2021 ◽  
Vol 131 ◽  
pp. 104016
Author(s):  
Yue-Fu Liu ◽  
Hua-Wen Qi ◽  
Xian-Wu Bi ◽  
Rui-Zhong Hu ◽  
Lin-Kun Qi ◽  
...  


Author(s):  
O.T. Woo ◽  
G.J.C. Carpenter

To study the influence of trace elements on the corrosion and hydrogen ingress in Zr-2.5 Nb pressure tube material, buttons of this alloy containing up to 0.83 at% Fe were made by arc-melting. The buttons were then annealed at 973 K for three days, furnace cooled, followed by ≈80% cold-rolling. The microstructure of cold-worked Zr-2.5 at% Nb-0.83 at% Fe (Fig. 1) contained both β-Zr and intermetallic precipitates in the α-Zr grains. The particles were 0.1 to 0.7 μm in size, with shapes ranging from spherical to ellipsoidal and often contained faults. β-Zr appeared either roughly spherical or as irregular elongated patches, often extending to several micrometres.The composition of the intermetallic particles seen in Fig. 1 was determined using Van Cappellen’s extrapolation technique for energy dispersive X-ray analysis of thin metal foils. The method was employed to avoid corrections for absorption and fluorescence via the Cliff-Lorimer equation: CA/CB = kAB · IA/IB, where CA and CB are the concentrations by weight of the elements A and B, and IA and IB are the X-ray intensities; kAB is a proportionality factor.



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