Contrasting detrital zircon age spectra in Cambrian sandstones, Taebaeksan Basin
ca. 500 Ma detrital zircon populations and juvenile whole-rock Nd signatures
Arc-related materials in Lower-Middle Cambrian sandstones, Taebaeksan Basin
“Neoproterozoic–early Cambrian” in Lee et al. (2016) is misleading.