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松辽盆地火山岩包裹体稀有气体同位素与天然气成因成藏示踪
引用本文:陶士振,戴金星,邹才能,王京红,米敬奎,汪泽成,胡素云. 松辽盆地火山岩包裹体稀有气体同位素与天然气成因成藏示踪[J]. 岩石学报, 2012, 28(3): 927-938
作者姓名:陶士振  戴金星  邹才能  王京红  米敬奎  汪泽成  胡素云
作者单位:中国石油勘探开发研究院;中国石油天然气股份有限公司油气储层重点实验室
基金项目:本文受国家大型气田与煤层气开发项目(2011ZX05001-001、2011ZX05004-001)资助.
摘    要:长期以来,国内外油气勘探主要是针对海相碳酸盐岩和海陆相碎屑岩,火山岩原来一直是油气勘探的禁区。松辽陆内裂谷盆地燕山期由于太平洋板块对中国大陆板块的斜向俯冲,发生弧后伸展裂陷,造成火山岩的大量喷发,以爆发相和溢流相为主。火山岩储层物性较好,不严格受埋深控制,但非均质性强,孔隙度0.5%~18.7%不等,渗透率0.0001×10-3~1×10-3μm2。火山岩裂缝内方解石脉或石英脉中包裹体捕获温度为105~250℃,多数在120~160℃;包裹体中气体3He/4He值分布在2.86×10-7~7.33×10-6,平均为2.48×10-6;R/Ra=0.26~5.24,多数R/Ra>1; 40Ar/36Ar=293~2485,主值区间为500~900;4He/20Ne=0.32~1255,主值区间为10~95和170~370;δ13C1=-17.1‰~-28.7‰,δ13C2=-23.4‰~-32.4‰,δ13Cco2=-10.97‰~-21.73‰。包裹体He、Ar、C等同位素数据表明,存在幔源通道,进而在火山岩中存在幔源无机成因气。根据火山岩产状和分布及其与断裂活动的关系,无机成因气藏主要分布于断裂带附近,有机成因气或有机-无机混源气则远离断裂活动带分布。本文包裹体同位素研究结果对确定松辽盆地深层火山岩储层中的天然气成因类型、分布规律,指导后续天然气勘探具有重要的参考价值。

关 键 词:包裹体  捕获温度  碳同位素  稀有气体同位素  火山岩  天然气成因和成藏  松辽盆地
收稿时间:2011-02-01
修稿时间:2012-01-02

The trace of genesis, formation and mineral resources of natural gas and rare gas isotope existing in volcanic inclusion of Songliao basin.
TAO ShiZhen,DAI JinXing,ZHOU CaiNeng,WANG JingHong,MI JingKui,WANG ZeCheng and HU SuYun. The trace of genesis, formation and mineral resources of natural gas and rare gas isotope existing in volcanic inclusion of Songliao basin.[J]. Acta Petrologica Sinica, 2012, 28(3): 927-938
Authors:TAO ShiZhen  DAI JinXing  ZHOU CaiNeng  WANG JingHong  MI JingKui  WANG ZeCheng  HU SuYun
Affiliation:PetroChina Research institute of Petroleum Exploration & Development, Beijing 100083, China;PetroChina Research institute of Petroleum Exploration & Development, Beijing 100083, China;PetroChina Research institute of Petroleum Exploration & Development, Beijing 100083, China;Key Laboratory for Oil & Gas Reservoirs of PetroChina, Beijing 100083, China;PetroChina Research institute of Petroleum Exploration & Development, Beijing 100083, China;PetroChina Research institute of Petroleum Exploration & Development, Beijing 100083, China;PetroChina Research institute of Petroleum Exploration & Development, Beijing 100083, China
Abstract:Ever since a long time ago,the oil-gas exploration home and aboard is mainly about marine facies carbonatite and sea and land facies clastic rock.Volcanic is always the forbidden area of exploration.In Yanshan Period,because of slant diving of pacific plate to Chinese continental plate,the rift basin in Songliao took place the back-arc stretch rift and causes the mass eruption of volcanic which is mainly eruption facies and overflowing facies.The quality of reservoir of volcanic is better and not strictly controlled by burial depth,but its anisotropy is obvious and porosity is 0.5%~18.7% and permeability is 0.0001×10-3~1×10-3μm2.The catching temperature of inclusion in calcite vein or quartz vein in crack of volcanic is 105~250℃,and majority is 120~160℃,and the 3He/4He specific value of gas in inclusion is 2.86×10-7~7.33×10-6 and the average number is 2.48×10-6.R/Ra=0.26~5.24,majority of R/Ra>1.40Ar/36Ar=293~2485 and the principle value interval is 500~900.4He/20Ne=0.32~1255,the principle value interval is 10~95 and 170~370.δ13C1=-17.1‰~-28.7‰,δ13C2=-23.4‰~-32.4‰,δ13Cco2=-10.97‰~-21.73‰.The data of He,Ar,C and other isotopes in inclusion reveal that there is mantle-genetic path,so there is mantle-genetic inorganic genetic gas in the volcanic.According to the attitude and distribution of volcanic and its relationship with rifting activity,inorganic genetic gas exists mainly around the rift vein and organic genetic gas or the mixture gas of inorganic genetic gas and organic genetic gas mainly exists far away from the rift vein.The research results of isotope in inclusion in this article have the significant reference value of confirming the genetic type and distribution of gas in the deep volcanic reservoir in Songliao basin and guiding the following exploration of natural gas.
Keywords:Inclusion  Catching temperature  Carbon isotope  Rare gas isotope  Volcanics  Genesis, formation and mineral resource of natural gas  Songliao basin
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