The regression of P 3 and (P 2 + N 2 ) values for the studied samples yield a positive trend with the coefficient R 2 of 0.93 (Fig. 8 E), supporting that samples in this study were derived from the same source rock.
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Tracking hydrothermal infiltration within light oil reservoirs using organic geochemical proxies in the Shunbei area of Tarim Basin in China.
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