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Hui Ye
Nanjing University
GeologyCratonArcheanPaleontologyPluton
2Publications
1H-index
2Citations
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Publications 3
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#1Hui Ye (NU: Nanjing University)H-Index: 1
#2Chang-Zhi Wu (NU: Nanjing University)H-Index: 11
Last. Weiqiang Li (NU: Nanjing University)H-Index: 15
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Abstract Equilibrium isotope fractionation factors are the basis for application of stable isotopes in geological studies. Experimental calibration and theoretical calculations have been employed to determine Fe isotope fractionation factors for a variety of minerals, however, these methods have their limitations. An alternative approach to calibrating inter-mineral Fe isotope fractionation factors is to use well-characterized geological samples; this approach has unique advantages over the othe...
1 CitationsSource
#1M.N. Muhtar (NU: Nanjing University)
#2Chang-Zhi Wu (NU: Nanjing University)H-Index: 11
Last. Lian-Xing Gu (NU: Nanjing University)H-Index: 12
view all 8 authors...
Source
#1Hui Ye (NU: Nanjing University)H-Index: 1
#2Chang-Zhi Wu (NU: Nanjing University)H-Index: 11
Last. Weiqiang Li (NU: Nanjing University)H-Index: 15
view all 8 authors...
Banded iron formations (BIFs) in Archean cratons provide important “geologic barcodes” for the global correlation of Precambrian sedimentary records. Here we report the first finding of late Archean BIFs from the Yangtze Craton, one of largest Precambrian blocks in East Asia with an evolutionary history of over 3.3 Ga. The Yingshan iron deposit at the northeastern margin of the Yangtze Craton, displays typical features of BIF, including: (i) alternating Si-rich and Fe-rich bands at sub-mm to met...
2 CitationsSource
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