渤海湾盆地渤中凹陷西南部深层烃源岩有机相预测

针对渤海湾盆地渤中凹陷西南部烃源岩层系多、非均质性较强等特点，开展了烃源岩干酪根显微组分、元素分析、岩石热解、气相色谱等地球化学分析测试，在沉积相的约束下对比了ΔlogR系列方法、多元回归法、BP神经网络法预测有机质丰度参数的优劣，优选BP神经网络法进行烃源岩总有机碳含量、裂解烃含量的单井预测，进而计算得到氢指数预测曲线，结合总有机碳含量进行有机相分析，定量刻画各层系烃源岩的有机相，分析烃源岩的优劣和展布特征。结果表明，BP神经网络法的预测精度相对较高，东营组二段下亚段烃源岩主要为Ⅱ₂型干酪根，氢指数为125～400 mg/g，总有机碳含量基本小于3%，其有机相主要为BC相、C相和CD相；东营组三段烃源岩主要为Ⅱ₁—Ⅱ₂型干酪根，沙河街组沙一二段、沙三段烃源岩主要为Ⅰ—Ⅱ₁型干酪根，这三套烃源岩的氢指数为250～650 mg/g，总有机碳含量为3%左右或大于3%，其有机相主要为B相、BC相和C相。沙河街组优质烃源岩主要发育于研究区中南部，是下一步勘探的重点区域。 

Prediction of organic facies of deep source rocks in southwestern part of Bozhong Sag,Bohai Bay Basin

Considering the characteristics of abundant source rock formations and heterogeneity in the southwestern part of the Bozhong Sag, Bohai Bay Basin, based on the geochemical and petrographic analysis of source rocks, the methods of ΔlogR series, multiple regression and BP neural network are applied to predict the organic matter abundance under the constraints of sedimentary facies.The BP neural network method is preferably used to predict the total organic carbon content and cracked hydrocarbon content of source rocks in a single well, and then the hydrogen index prediction curve is calculated.Combined with total organic carbon content,the organic phase of each source rock layer is quantitatively described, and the advantages and disadvantages and distribution characteristics of source rocks are analyzed. Results show that the prediction accuracy of BP neural network method is relatively higher. The source rocks in the lower section of the second member of Dongying Formation are featured by kerogen of type Ⅱ₂, hydrocarbon index of 125-400 mg/g, TOC content basically less than 3%, and organic facies of BC, C and CD types. The source rocks in the third member of Dongying Formation are featured by kerogen of typesⅡ₁ to Ⅱ₂. The source rocks in the first, second and third members of Shahejie Formation are featured by kerogen of types Ⅰ to Ⅱ₁, TOC content about 3% or higher than 3%, and organic facies of B, BC and C types.The high-quality source rocks of the Shahejie Formation are mainly developed in the central and southern parts of the study area, and are the key areas for further exploration.