Vol. 308, Issue 3, 2008March 01, 2008 EDT
SHRIMP U-Pb and CAMECA 1280 Oxygen Isotope Results From Ancient Detrital Zircons in the Caozhuang Quartzite, Eastern Hebei, North China Craton: Evidence for Crustal Reworking 3.8 Ga Ago
SHRIMP U-Pb and CAMECA 1280 Oxygen Isotope Results From Ancient Detrital Zircons in the Caozhuang Quartzite, Eastern Hebei, North China Craton: Evidence for Crustal Reworking 3.8 Ga Ago
Simon A. Wilde, John W. Valley, Noriko T. Kita, Aaron J. Cavosie, Dunyi Liu,
Wilde, S. A., Valley, J. W., Kita, N. T., Cavosie, A. J., & Liu, D. (2008). SHRIMP U-Pb and CAMECA 1280 Oxygen Isotope Results From Ancient Detrital Zircons in the Caozhuang Quartzite, Eastern Hebei, North China Craton: Evidence for Crustal Reworking 3.8 Ga Ago. American Journal of Science, 308(3), 185–199. https://doi.org/10.2475/03.2008.01