Geology record of mantle-derived magmatogenetic CO2 gas in the northeastern China

doi:10.7623/syxb201001010

Editorial office of ACTA PETROLEI SINICA ›› 2010, Vol. 31 ›› Issue (1): 61-67.DOI: 10.7623/syxb201001010

• Petroleum Exploration • Previous Articles Next Articles

Geology record of mantle-derived magmatogenetic CO₂ gas in the northeastern China

QU Xiyu 1 LIU Li 1 GAO Yuqiao 2 LIU Na 1 LI Fulai 1 LIU Hongyan 3

Received:2009-02-22 Revised:2009-06-20 Online:2010-01-25 Published:2010-05-21
Contact: QU Xiyu

中国东北地区幔源-岩浆CO₂赋存的地质记录

曲希玉 1 刘立 1 高玉巧 2 刘娜 1 李福来 1 刘红艳 3

1吉林大学地球科学学院吉林长春 130061； 2南京大学内生金属矿床成矿机制研究国家重点实验室江苏南京 210093； 3吉林大学测试科学实验中心吉林长春 130061

通讯作者: 曲希玉

Abstract

Abstract:

The relationship between the genesis of CO₂ and dawsonite in the northeastern China was studied on the base of the research of CO₂ gas reservoirs and dawsonite in the south of Songliao Basin and Hailaer Basin,with the help of the analysis of carbon and helium isotopes of CO₂ gas reservoirs and carbon-oxygen isotopes of dawsonite in each basin respectively,and combining with the relationship between CO₂ gas reservoirs and fault,volcanic rocks.It was found that most of CO₂ in the northeastern China had a mantle-derived magmatic genesis and was homology with the CO₂ forming the dawsonite.As the trace mineral for CO₂,dawsonite can register the accumulation of CO₂ during geological history.High concentration of Na⁺，K⁺，HCO₃^-and CO₃^2-were displayed owing to the modification of CO₂ in formation water and crude oil.The geology record of mantle-derived magmatogenetic CO₂ was built according to the relationship between dawsonite and CO₂,the changing on the concentration of the ion in formation water and the abundant CO₂ dissolving in crude oil.

Key words: Northeastern China, mantle-derived magmatogenetic CO₂, dawsonite, formation water, crude oil

摘要：

在松辽盆地南部及海拉尔盆地CO₂气藏和片钠铝石研究的基础上，根据中国东北地区CO₂气藏中CO₂的碳同位素、氦同位素，各盆地片钠铝石的碳、氧同位素的数据，以及CO₂气藏（苗）与断裂和火山岩的关系，对中国东北地区CO₂的成因及其与片钠铝石的关系进行了研究。分析认为中国东北地区的CO₂绝大多数为幔源-岩浆成因，且形成片钠铝石的CO₂与幔源-岩浆CO₂同源；片钠铝石是CO₂的“示踪矿物”，记录了地质历史时期CO₂的聚集；地层水和原油中溶有大量的无机成因CO₂，经CO₂改造的地层水具有高矿化度及Na⁺ 、K⁺ 、HCO₃^-、CO₃^2-浓度高的特点。依据片钠铝石与CO₂的关系，地层水中离子浓度的变化，以及原油中溶解大量CO₂的事实，总结了中国东北地区幔源-岩浆CO₂赋存的地质记录。

关键词: 中国东北地区, 幔源-岩浆CO₂, 片钠铝石, 地层水, 原油

QU Xiyu LIU Li GAO Yuqiao LIU Na LI Fulai LIU Hongyan. Geology record of mantle-derived magmatogenetic CO₂ gas in the northeastern China[J]. Editorial office of ACTA PETROLEI SINICA, 2010, 31(1): 61-67.

曲希玉刘立高玉巧刘娜李福来刘红艳. 中国东北地区幔源-岩浆CO₂赋存的地质记录[J]. 石油学报, 2010, 31(1): 61-67.

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Geology record of mantle-derived magmatogenetic CO₂ gas in the northeastern China

中国东北地区幔源-岩浆CO₂赋存的地质记录

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