Comments on “Detrital zircon geochronology and Nd isotope geochemistry of the basal succession of the Taebaeksan Basin, South Korea: Implications for the Gondwana linkage of the Sino-Korean (North China) Block during the Neoproterozoic-early Cambrian” by Lee et al. [Palaeogeography, Palaeoclimatology, Palaeoecology 441 (2016) 770-786]
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文摘

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.

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