The Wenchang B depression and the western Qionghai uplift, in the south of the Zhu-3 sub-basin, are two adjacent sub-tectonic units with multiple oil-bearing structures. The former contains well-developed source rocks, whereas the latter does not. Previous studies have preliminarily explored the source of crude oil in the Wenchang B depression and the western Qionghai uplift. However, systematic investigations have been absent in characterizing the two main source rocks (i.e. Enping and Wenchang formations) and elucidating the migration of crude oil, which has significantly hindered oil and gas exploration. In this study, multiple methods are integrated to re-evaluate the source rocks of the depression, clarify crude oil sources, and analyse vertical oil migration and accumulation characteristics. The methods used included Rock-Eval pyrolysis, carbon isotope analysis, gas chromatography-mass spectrometry (GC-MS), hierarchical cluster analysis (HCA), and basin modelling. The source rocks of the Wenchang formation are demonstrated to have good to excellent hydrocarbon generation potential, whereas those of the Enping Formation have fair to good potential. Both source rocks are further divided into two members (i.e. EP1 and EP2 members for the Enping Formation and WC1 and WC2 members for the Wenchang Formation) based on differences in the biomarkers including ratios of bicadinanes (W + T)/C30hopane (C30H), ∑C30 4-methylsterane (MSt)/∑C29 regular sterane (RSt), pristane (Pr)/phytane (Ph), and ∑C27RSt/∑C29RSt, the source rocks are divided into four sets, named E1, E2 of the Enping Formation, and W1, W2 of the Wenchang Formation, respectively. Both W1 and W2 source rocks were weakly oxidizing-weakly reducing sedimentary environments. The input of organic matter to W2 source rock was dominated by aquatic organisms such as algae. The parent source of W1 source rock has both the contribution of aquatic organisms and the input of terrestrial organic matter. The E1 source rock was formed in an oxidative depositional environment, and its parent source is similar to that of W1. E2 source rock was a weakly oxidizing-weakly reducing depositional environment, and the parent source was resins from higher plants. There are great differences in crude oil characteristics. Through HCA and oil-source correlation analysis, the crude oil in the Wenchang B depression was found to be mainly from the W2 source rock. However, in the northern part of the depression, some crude oil was suggested to originate from both W1 and E1 source rock, presenting mixed characteristics. The crude oil in the western Qionghai uplift was mainly derived from W1 and E1 source rocks, with a small part was from the W2 source rock.
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