SUN Xingli; CHEN Jianfa; LIU Wenhui and WANG Darui
, 2004, 31(3): 830-0.
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In marine sedimentary strata of the Tarim Basin, Northwest China, Yurtusi Formation, Lower Cambrian has been proved to be one of the main source rocks. Laminar cherts intercalated with black shale in outcrops of the Yurtusi Formation. The content of As, Sb, Hg, Ba, Sr, V, Ni, Mo and U are rich in the cherts, especially, As, Hg, Ba and U are much richer. The ratio of Ba/Sr is lower than 10×104, and U/Th ratio is greater than 1. The ∑REE of cherts are lower, with obviously negative anomaly normalized by North America Shale, in which δCe and Lan/Cen values are 0.524-0.991 and 1.112-2.934, respectively. The geochemical characteristics suggest that cherts are likely deposited with a hydrothermal origin and formed in continental margin-abyssal environment and developed with the black shale that is deposited in anoxic environment and anoxic event.