Palaeoenvironment and its control on the formation of Miocene marine source rocks in the Qiongdongnan Basin, northern South China Sea.

For example, data from three wells (YC35-1-2, LS15-1-1, and ST36-1-1) drilled in the margin of the central depression reveals an increasing trend of TOC of the Miocene marine source rocks from the shallow to relatively deeper water ( Figure 3 ). 4.2.

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