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Dong CY, Wan YS, Xu ZY, Liu DY, Yang ZS, Ma MZ, Xie HQ, 2013. Late Paleoproterozoic kondalites in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating. Science China Earth Sciences, 56: 115–125.
Liu SJ, Dong CY, Xu ZY, Santosh M, Ma MZ, Xie HQ, Liu DY, Wan YS, 2013. Paleoproterozoic episodic magmatism and high-grade metamorphism in the North China Craton: Evidence from SHRIMP zircon dating of magmatic suites from the Daqingshan area. Geological Journal, 48: 429–455.
Wan YS, Xu ZY, Dong CY, Nutman A, Ma MZ, Xie HQ, Liu DY, Wang HC, Cu H, 2013. Episodic Paleoproterozoic (~2.45, ~1.95 and ~1.85 Ga) mafic magmatism and associated high temperature metamorphism in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating and whole-rock geochemistry. Precambrian Research, 224, 71– 93.
Wan YS, Zhang YH, Williams IS, Liu DY, Dong CY, Fan RL, Shi YR, Ma MZ, 2013. Extreme zircon O isotopic compositions from 3.8 to 2.5 Ga magmatic rocks from the Anshan area, North China Craton. Chemical Geology, 352: 108–124.
Wan YS, Xie HQ, Yang H, Wang ZJ, Liu DY, Kroner A, Wilde SA, Geng YS, Sun LY, Ma MZ, Liu SJ, Dong CY, Du LL, 2013. Is the Ordos Block Archean or Paleoproterozoic in age? Implications for the Precambrian evolution of the North China Craton. American Journal of Science, 313: 683–711.
Liu SJ, Wan YS, Sun HY, Nutman A, Xie HQ, Dong CY, Ma MZ, Du LL, Liu DY, 2013. Paleo- to Eoarchean crustal materials in eastern Hebei, North China Craton: New evidence from SHRIMP U-Pb dating and in-situ Hf isotopic studies in detrital zircons of supracrustal rocks. Journal of Asian Earth Sciences, 78: 4–17.
Dong CY, Wan YS, Wilde SA, Xu ZY, Ma MZ, Xie HQ, Liu DY, 2014. Early Paleoproterozoic supracrustal rocks at Daqingshan in the Khondalite Belt of North China Craton: Evidence from SHRIMP zircon U-Pb dating. Gondwana Research, 25: 1535–1553.
Wan YS, Xie SW, Yang CH, Kröner K, Ma MZ, Dong CY, Du LL, Xie HQ, Liu DY, 2014. Early Neoarchean (~2.7 Ga) tectono-thermal events in the North China Craton: A synthesis. Precambrian Research, 247: 45–63.
Wan YS, Dong CY, Wang SJ, Kröner A, Xie HQ, Ma MZ, Zhou HY, Xie SW, Liu DY, 2014. Middle Neoarchean magmatism in western Shandong, North China Craton: SHRIMP zircon dating and LA-ICP-MS Hf isotope analysis. Precambrian Research, 256: 865–884.
Wan YS, Zhao XZ, Wang ZJ, Liu DY, Kröner A, Dong CY, Xie HQ, Geng YS, Zhang YH, Fan RL, Sun HY, 2014. SHRIMP zircon dating and LA-ICPMS Hf analysis of early Precambrian rocks from drill holes into the basement beneath the Central Hebei Basin, North China Craton, Geoscience Frontiers, 5: 471–484.
Xie SW, Xie HQ, Wang SJ, Kröner A, Liu SJ, Zhou HY, Ma MZ, Dong CY, Liu DY, Wan YS, 2014. Ca. 2.9 Ga granitoid magmatism in eastern Shandong, North China Craton: Zircon dating, Hf-in-zircon isotopic analysis and whole-rock geochemistry. Precambrian Research, 255: 538–562.
Wan YS, Liu DY, Dong CY, Xie HQ, Kröner A, Ma MZ, Liu SJ, Xie SW, Ren P, 2015. Formation and evolution of Archean continental crust of the North China Craton. In: Zhai MG (Ed.) Precambrian geology of China. Springer, 59–136.
Wan YS, Ma MZ, Dong CY, Xie HQ, Xie SW, Ren P, Liu DY, 2015. Widespread late Neoarchean reworking of Meso- to Paleoarchean continental crust in the Anshan-Benxi area, North China Craton, as documented by U-Pb-Nd-Hf-O isotopes. American Journal of Science, 315: 620–670.
Wan YS, Liu SJ, Kröner A, Dong CY, Xie HQ, Xie SW, Bai WQ, Ren P, Ma MZ, Liu DY, 2016. Eastern Ancient Terrane of the North China Craton. Acta Geologica Sinica, 90: 1801–1840.
Wan YS, Liu DY, Xie HQ, Kröner A, Ren P, Liu SJ, Xie SW, Dong CY, Ma MZ, 2016. Formation ages and environments of Early Precambrian banded iron formation in the North China Craton. In: Zhai MG (Ed.) Main tectonic events and metallogeny of the North China Craton. Springer, 65–83.
Ren P, Xie HQ, Wang SJ, Nutman AP, Dong CY, Liu SJ, Xie SW, Che XC, Song SY, Ma MZ, Liu DY, Wan YS, 2016. Ca. 2.6 Ga tectono-thermal event in western Shandong Province, North China Craton: Evidence from SHRIMP zircon U-Pb dating and O isotope analysis. Precambrian Research, 281: 236–252.
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