DYNAMIC ACCUMULATION PROCESS OF COAL-FORMED GAS IN WENLIU AREA, DONGPU DEPRESSION
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摘要: 文留地区是渤海湾盆地典型的煤成气区之一,随着勘探认识的不断深入,研究区煤成气运聚成藏过程的精细刻画仍需完善。运用流体包裹体技术分析文留地区煤成气成藏时间,基于断层活动特征明确研究区输导体系演化特征,根据断—盖组合关系及烃类流体包裹体丰度(GOI)测试结果分析气藏保存条件,最终明确文留地区煤成气成藏过程。研究表明,文东断层为研究区气源断层,其输导供烃条件可用断层输导效率系数(FTEC)进行量化表征,评价结果表明研究区具有优越的气源供给条件;文留地区煤成气来源于临近的洼陷带,煤成气在东营组沉积时期沿文东断层垂向运移至石炭—二叠系和沙四段储层聚集成藏,东营末构造抬升期气藏受构造运动影响而发生少量天然气散失。Abstract: The Wenliu area is one of the typical coal-formed gas accumulation zones in the Bohai Bay Basin. With the deepening of exploration, the fine characterization of the coal-forming gas accumulation process in this area still needs to be improved. The fluid inclusion technology was used to analyze the coal-formed gas accumulation date in Wenliu area. Based on the analysis of fault activity, the evolution characteristics of the transport system in the study area were determined. The gas-fluid inclusion abundance (GOI) test were used to analyze the gas preservation conditions, and finally the process of coal-formed gas accumulation in Wenliu area was carried out. The results show that the Wendong fault is a gas source fault in the study area, and its hydrocarbon supply conditions can be characterized by the Fault Transport Efficiency Coefficient (FTEC). The study area has superior gas supply conditions; the coal-formed gas in Wenliu area originates from the adjacent deep sag zone, and vertically transports along the Wendong fault to the Carboniferous-Permian and the Es4 sandstone reservoirs in the trap during the sedimentary period of the Dongying Formation. Small amount of the coal-formed gas loss occurred during the tectonic uplifting movements in the late sedimentary period of the Dongying Formation.
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Table 1. Components and carbon isotope data of natural gas in the Wenliu area
井号 井深/m 层位 组分含量/% 干燥系数 碳同位素组成/‰ Ro 甲烷 乙烷 丙烷 异丁烷 正丁烷 异戊烷 正戊烷 CO2 N2 C1/C1-4 C1 C2 C3 文理108-7 2016.1~3092.8 Es4 95.34 1.62 0.56 0.11 0.17 0.07 0.09 0.82 1.03 0.97 -28.00 -24.60 -25.50 2.83 文23-25 2950.4~2992.5 Es4 96.19 1.60 0.43 0.10 0.14 0.05 0.05 0.49 0.86 0.98 -28.00 -24.60 -25.40 2.83 文108-5 3070~3165.1 Es4 91.10 1.59 0.67 0.15 0.26 0.15 0.21 0.14 5.29 0.97 -28.00 -24.50 -25.50 2.83 文69-9 2933.8~2983 Es4 94.31 1.52 0.45 0.09 0.13 0.05 0.06 0.41 2.87 0.98 -28.10 -24.50 -26.00 2.79 文23-11 2930~2940 Es4 95.99 1.57 0.46 0.09 0.15 0.05 0.06 0.73 0.81 0.98 -28.10 -24.60 -26.00 2.79 文109 2746~2920.8 Es4 95.91 1.59 0.41 0.09 0.14 0.04 0.05 0.44 1.22 0.98 -28.10 -24.60 -25.70 2.79 文23-3 2881.9~3008.5 Es4 96.00 1.59 0.43 0.09 0.13 0.04 0.05 0.66 0.90 0.98 -28.00 -24.90 -25.60 2.83 文23 2813.2~3026.5 Es4 96.75 1.82 0.43 0.69 0.98 -29.00 -23.30 -21.40 2.41 文古2 3813.5~3834.0 P2sh 93.36 2.58 0.29 0.84 0.94 -29.60 -24.30 -21.40 2.18 注:戴金星煤成气δ13C1-Ro关系式:δ13C1=14.12lgRo-34.39 表 2 气源断层与源岩静态配置关系数据表
Table 2. Static configuration data of gas source fault and source rocks
煤成气区 气源断层 平均生气强度I/(×108 m3/km2) 气源断层接触源岩长度L/km 气源断层接触烃源岩深度H/km 气源断层接触面积s/km2 接触面积总计S/km2 煤成气探明储量/(×108 m3) 断层输导效率系数FTEC 文23 文东 33 15.96 2.52 40.22 57.96 149.4 1912.68 文东派生 11.67 1.52 17.74 户部寨 卫西 28 9.58 0.72 6.9 28.71 43.91 803.88 卫西派生1 8.11 1.12 9.08 卫西派生2 3.76 1.16 4.36 濮城 11.79 0.71 8.37 白庙 兰聊 35 8.59 2.67 22.94 22.94 35.11 802.9 马厂 马东1号 25 8.4 1.37 11.51 19.66 10.47 491.5 马东2号 7.28 1.12 8.15 -
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