Geochemical characteristics of the lower part of Shayi Member in Lixian Slope,Raoyang Sag,Bohai Bay Basin,Northern China: Implications for organic matters origin,thermal maturity and depositional environment |
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| Authors: | Fugui He Xianzhi Gao Xianzheng Zhao Dexiang Yang XueJun Lu Jingwang Liu Xiongying Dong Huilai Wang Dongsheng Wu |
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| Institution: | 1.College of Geosciences in China University of Petroleum,Beijing,China;2.State Key Laboratory of Petroleum Resources and Prospecting,Beijing,China;3.Dagang Oilfield Branch Company, PetroChina,Tianjing,China;4.Huabei Oilfield Branch Company, PetroChina,Renqiu,China;5.College of Geosciences in Yangtze University,Wuhan,China |
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| Abstract: | The lower part of Shayi Member (Es1x Sub-Member) composed mainly of dark mudstones and shales is the dominant source rocks for the Lixian Slope. Based on organic petrology, organic and inorganic geochemistry analyses of several mudstone and shale samples selected from Es1x Sub-Member, this research provides an overview on type, origin and thermal maturity of organic matters, as well as depositional environment of Es1x Sub-Member. Kerogen microscopy observation shows that the macerals are dominated by sapropelinite with a significant mixture of vitrinite and inertinite, indicating that aquatic algal-bacterial organic matter inputs are dominate with a significant contribution of terrigenous organic matter inputs. This statement is supported by n-alkane patterns distribution characteristics, high (n-C21 + n-C22)/(n-C28 + n-C29) values (average = 1.77), the plot of high Ph/n-C18 values (average = 4.15) versus low Pr/n-C17 values (average = 1.13), and high proportion of C27 sterane and C29 sterane (average = 37.7 and 42.0%, respectively). In addition, the rather low Pr/Ph values (average = 0.38), high gammacerane index values (average = 0.30), high V/Ni and V/(V + Ni) values (average = 11.84 and 0.89, respectively), high Sr/Ba and Sr/Cu values (average = 8.54 and 108, respectively), indicative of a saline water condition and a anoxic depositional environment. The low C29 sterane ααα 20S/(20S + 20R), C29 sterane αββ/(αββ + ααα), C31 homohopane 22S/(22S + 22R), C32 homohopane 22S/(22S + 22R), Ts/(Ts + Tm) values and relatively high moretane/hopane values show that the level of thermal maturity of organic matters in Es1x Sub-Member are low. |
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