Predicting Source Rock Distribution of the Ninth Member of the Upper Triassic Yanchang Formation Based on Well-Logging Parameters and TOC Values in the Longdong Area, Ordos Basin, China.

(2) The organic-rich source rocks belong to the noneasily conductive materials, which lead to the RT showing an increasing trend with the TOC ( Figure 5 b).

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In the map of the Chang 9 source rock predicted by our model, the thickness of the source rock (TOC ≥ 1.0%) varies in the range of 1–12 m, showing a decreasing trend from northeast to southwest in the Longdong area.

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