Distribution and Major Controlling Factors of CO2 Reservoirs in Lishui Sag, East China Sea Basin
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摘要: 基于丽水凹陷钻井和地震资料,综合天然气地球化学参数、基底断裂和岩浆底辟发育特征等,研究丽水凹陷CO2的分布特征及其成藏主控因素.研究结果表明,丽水凹陷CO2纵向上主要分布在灵峰组、明月峰组下段及元古界基底片麻岩中,不同层位CO2的含量差别很大;平面上,温州13-1、丽水35-7和南平5-2 CO2气藏均位于岩浆底辟体之上或者附近,同时周围亦发育断层,而丽水36-1高含CO2气藏和LF-1井含CO2气藏周围底辟不发育,均紧邻灵峰凸起西侧的控洼断裂.丽水凹陷幔源CO2成藏主要受早中新世和晚中新世两期火山岩浆活动的影响,这两期火山活动将幔源CO2带到地壳浅层,通过砂体侧向输导进入有利圈闭聚集成藏.Abstract: Based on the drilling data and seismic data of Lishui sag, the distribution and major controlling factors of CO2 reservoirs are studied by combining geochemical parameters of natural gas and development characteristics of basement faults and magma diapirs. The results show that CO2 is mainly concentrated in Lingfeng Formation, lower segment of Mingyuefeng Formation and Proterozoic basal gneiss in the vertical. Besides, the content of CO2 varies greatly in different layers. Laterally, Wenzhou 13-1, Lishui 35-7 and Nanping 5-2 structural CO2 gas reservoirs are located on or near the magma diapirs, and there are faults around these CO2 gas reservoirs. Whereas, there is no diapir near Lishui 36-1 structural CO2 gas reservoirs and LF-1 containing CO2 gas reservoir, but they are adjacent to large depression-controlling faults which are located at west side of Lingfeng uplift. The distribution of CO2 gas reservoirs in the Lishui sag is mainly controlled by two stages magmatic activities, which are respectively in Early Miocene and Late Miocene. Mantle-derived CO2 gas is carried by the deep volcanic magma activities to shallow crust, then migrates along with sand body to favorable traps and forms CO2 gas pools.
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图 2 丽水凹陷地层及构造演化
据仝志刚等(2012)、张田等(2015)和蒋一鸣等(2020)修编
Fig. 2. Stratigraphic and tectonic evolution of Lishui sag
图 3 丽水凹陷CO2有机与无机成因判别
Fig. 3. Identification of organic or inorganic origin of CO2 in Lishui sag
图 7 南平5-2构造及温州13-1构造CO2气藏地震剖面解析
图例同图 5
Fig. 7. Seismic section analysis of Nanping 5-2 and Wenzhou 13-1 structure CO2 gas reservoirs
表 1 丽水凹陷天然气地球化学参数
Table 1. Geochemical parameters of natural gas in Lishui sag
井名 地层 深度(m) 气体主要组分(%) 碳同位素(‰) R/Ra 3He/ 4He(10-7) 数据来源 CH4 C2+ N2 CO2 δ13CCO2 SMT-1 E1l 2 571~2 589 1.62 0.85 0.67 95.63 -4.15 苏奥等,2014
何家雄等,2005
黄志龙等,20032 638~2 657 0.42 - 0.29 99.42 -4.19 WZ13-1-1 E1l 3 335~3 345 4.76 0.76 94.47 -4.00 7.20 101.00 3 405~3 412 1.19 0.22 98.59 -4.20 8.80 123.00 3 641~3 666 0.13 99.87 -4.20 5.40 75.00 LS36-1-1 E1m 2 251~2 283 55.45 6.85 3.55 34.15 -5.03 55.10 6.75 3.44 34.50 -4.67 LF-1 基底 2 511~2 530 59.48 6.16 痕量 -22.20 苏奥等,2014
黄志龙等,2003
葛和平等,2007LS36-1-2 E1m2 2 238~2 260 56.52 10.68 1.06 31.74 -4.60 8.80 59.70 -
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