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Characteristics of noble gases in the large Gaoshiti-Moxi gas field in Sichuan Basin, SW China

机译:中国西南地区四川盆地高石梯—磨溪气田稀有气体特征

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Taking the large Gaoshiti-Moxi gas field of Sichuan Basin as an example, the total composition contents and isotopes of noble gases in the natural gases from the Sinian Dengying Formation and Cambrian Longwangmiao Formation are analyzed, and then their geneses are identified. The content value of helium in the natural gases of the large Gaoshiti-Moxi gas field is generally 1-2 orders of magnitude higher than that of air, and the average content in the second member of the Dengying Formation is 512×10?6, reaching the industrial utilization standard. The content values of Neon, Argon, Krypton and Xenon are relative low, lower than the corresponding content value in air. The total composition contents of noble gases in the natural gas of the large Gaoshiti-Moxi gas field gradually reduce in the sequence of the second member of Dengying Formation, the fourth memeber of Dengying Formation, and Cambrian Longwangmiao Formation. The noble gases3He/4He value in the natural gases of the large Gaoshiti-Moxi gas field is in 10?8order of magnitude, the40Ar/36Ar value is usual from 1 024 to 9 559,132Xe is relatively surplus and129Xe is relatively loss. The comprehensive genetic identification of Helium, Argon, Xenon indicates that the noble gases in the large Gaoshiti-Moxi gas field are typical crustal source genesis, and the study area has stable tectonic background and does not have active deep fractures or mantle connecting fractures.
机译:以四川盆地高石梯—磨溪气田为例,分析了震旦系灯影组,寒武纪龙王庙组天然气中的总成分含量和稀有同位素,并确定了它们的成因。大高石梯—磨溪气田天然气中的氦含量一般比空气高1-2个数量级,灯影组第二段平均含量为512×10?6,达到工业利用标准。氖,氩,K和氙的含量值相对较低,低于空气中的相应含量值。大高石梯—磨溪气田天然气中稀有气体的总组成含量按灯影组第二段,灯影组第四段和寒武纪龙王庙组的顺序逐渐减小。大高石梯—莫溪气田天然气中的稀有气体3He / 4He值在10-8个数量级,40Ar / 36Ar值通常在1,024至9,559,132Xe相对过剩,129Xe相对损耗。对氦气,氩气,氙气的综合遗传鉴定表明,高石梯—磨溪气田中的稀有气体是典型的地壳成因,研究区具有稳定的构造背景,没有活跃的深部裂缝或地幔连接裂缝。

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