Fig. 2 | Scientific Reports

Fig. 2

From: Geochemical characteristic of different-lithofacies source rocks and its implications for ultradeep hydrocarbon exploration in the lower cambrian Yuertus formation, Tarim basin

Fig. 2The alternative text for this image may have been generated using AI.

(a) Evaluation of organic matter abundance in Є1y source rocks in different regions of the Tarim Basin. (Data sources: LT1 (Zhu et al.22); LT3 (Ai et al.40); YD2 (Ying et al.41); XH1 (Zhu et al.42); (b) Evaluation of kerogen types in Є1y source rocks in the Tarim Basin. (Data sources: XH1, DEG, SGTBLK, XE(Chen et al.35); YD2 (Ying et al.41); TD2 (Liu et al.43); (c) Evaluation of organic matter thermal evolution in Є1y source rocks in the Tarim Basin. (Data sources: KLX (Yang et al.44); XE (Yu et al.45); KGKT (Ouyang et al.46; Zhang et al.47); SGTBLK (Zhang et al.47); XH1 (Zhu et al.42); QT1 (Zhang et al.21); LT1 (Zhu et al.22); YD2, TD1, TD2 (Liu et al.43).

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