Characteristics and significance of the solid bitumen in the second member of Dengying Formation of Sinian system in the north of central Sichuan Basin, China

Xingzhi Ma , Bokai Dai , Shaobo Liu , Xuesong Lu , Junjia Fan , Qiang Liu , Fan Yang
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Abstract

With ongoing advancements in natural gas exploration, the second member of the Sinian Dengying Formation (Deng 2 Member) has emerged as a crucial region for providing natural gas reserves in the north of the central Sichuan Basin. The Deng 2 Member has a significant volume of reservoir solid bitumen. Geochemical characteristics and development mechanism of the solid bitumen were determined through measurements and analyses of the Deng 2 Member samples collected from primary exploration wells by using optical microscopy, SEM, gas chromatograph-mass spectrometer, and laser Raman spectrometer. The results show that the Deng 2 Member has a generally high content of solid bitumen, ranging from 2.96% to 5.13% on average in single wells. The solid bitumen mainly occurs as the fillings of dissolved pores (caves) and fractures, followed by intergranular pores, in the shape of spots, balls, plates, and veins dominantly. Diasteranes content and laser Raman spectrograms indicate that the solid bitumen is in the high maturity stage. The bitumen reflectance calculated by laser Raman spectroscopy is distributed between 2.49% and 4.09%, indicating the major source of the thermal cracking of crude oil. Solid bitumen in the Deng 2 Member has different contents of 21α(H)–C29 norhopane, C35 hopane, and C34 hopane, and Ts/Tm values from the Deng 4 Member in the Gaoshiti Moxi area. It is inferred that some solid bitumen is from the source rocks of the Lower Cambrian Maidiping Formation and the Sinian Doushantuo Formation. Two stages of bitumen were developed in the Deng 2 Member, indicating possible two stages of oil filling and thermochemical sulfate reduction (TSR) in the geologic history.

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川中北部震旦系灯影组二段固体沥青的特征及意义
随着天然气勘探的不断深入,震旦系邓营组二段(邓二段)已成为川中盆地北部重要的天然气储量区。邓二段储层固体沥青储量较大。利用光学显微镜、扫描电镜、气相色谱-质谱仪和激光拉曼光谱仪对邓二段初探井样品进行了测定和分析,确定了固体沥青的地球化学特征和形成机理。结果表明,邓二段固体沥青含量普遍较高,单井平均含量在2.96%~5.13%之间。固体沥青主要以溶解孔隙(洞穴)和裂缝的填充物出现,其次是粒间孔隙,主要呈点状、球状、板状和脉状。二甾烷含量和激光拉曼光谱图表明,该固体沥青处于高成熟期。激光拉曼光谱计算的沥青反射率分布在2.49%至4.09%之间,表明原油热裂解的主要来源。邓2段固体沥青中21α(H)–C29 norhopane、C35 hopane和C34 hopane的含量与高石梯磨溪地区邓4段的Ts/Tm值不同。推测部分固体沥青来源于下寒武统麦地坪组和震旦系陡山沱组烃源岩。邓2段沥青发育了两个阶段,表明地质史上可能存在两个充油和热化学硫酸盐还原阶段。
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