Elemental Geochemical Characteristics of Shales from Wufeng-Longmaxi Formations in the Southern Margin of the Qinling Orogenic Belt, China: Implications for Depositional Controls on Organic Matter.

Since the TOC content in the Bajiaokou profile is generally lower, the positive effect of this debris flux on the TOC may not be significant.

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The Zr content showed a trend of first increasing and then decreasing, with a content of 181.30–231.60 μg/g (average 208.45 μg/g).

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