天然气地球化学

济阳坳陷渤南洼陷深层天然气的地球化学特征及成因探讨

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  • 1.中国石化胜利油田有限公司勘探事业部,山东 东营 257000
宋明水(1964-),男,山东沾化人,博士,高级工程师,主要从事油气勘探研究和管理工作.

收稿日期: 2004-10-08

  修回日期: 2004-10-08

  网络出版日期: 2004-12-20

DISCUSSION ON DEEP GAS GEOCHEMICAL CHARACTERISTICS AND GENESIS OFBONAN SAG, JIYANG DEPRESSION

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  • Exploration Department of Shengli Oilfield Company, SINOPEC, Dongying  257000, China

Received date: 2004-10-08

  Revised date: 2004-10-08

  Online published: 2004-12-20

摘要

通过对济阳坳陷渤南洼陷深层天然气的组分及其碳、氢同位素和稀有气体同位素组成的研究表明:该洼陷天然气重烃含量较高,显示出正常的原油伴生气的特征,不应为来源于高成熟―过成熟源岩的天然气;天然气的碳、氢同位素组成特征显示该区深层天然气为生物气、油型气和煤成气3种不同类型混合的天然气。另外,通过对渤南洼陷深层天然气中稀有气体氦同位素的分析,表明该区伴生气为典型的壳源成因,幔源挥发份加入的现象不明显,深层断裂活动也不发育,是在深层聚集成藏的天然气。

本文引用格式

宋明水, 张学才 . 济阳坳陷渤南洼陷深层天然气的地球化学特征及成因探讨[J]. 天然气地球科学, 2004 , 15(6) : 646 -649 . DOI: 10.11764/j.issn.1672-1926.2004.06.646

Abstract

According to the chemical composition, carbon isotope, hydrogen isotope and noble gas isotope researches, the deep gas of Bonan sag displayed the characteristics of normal accompanying gas with crude  oil, with high contents of heavy hydrocarbons. The genesis of the deep gas may not be high mature to over mature source rocks. The characteristics of carbon and  hydrogen isotope composition show that the deep gas of Bonan sag mixed by biogenic gas, thermgenic gas and coal-formed gas. The noble gas (He) isotope of the  deep gas from Bonan sag indicated that the accompanying gas with crude oil in the sag is typical crust type gas, without clear mantle type gas. Based on the low  frequency of deep fault activity, Bonan sag provided a advantaged geologic area for deep oil and gas accumulation.

参考文献

[1]Berner U, Faber E.Maturity related mixing model for meth ane, ethane and propane, based on carbon isotopes[J]. Org Geochem, 1988,13: 67-72.
[2] Fuex A N. The use of stable carbon isotopes in hydrocarbon exploration[J]. Geochem Explor, 1977,7:155-188.
[3] Galimov E. Source and mechanisms of formation of gaseous hydrocarbons in sedimentary rock[J]. Chemical Geology, 1988,(1-3):77-95.
[4] James A T. Correlation of natural gas by use of carbon isot opic distribution between hydrocarbon components[J]. Am Assoc Geol Bull,1983, 67:1176-1191.
[5] Manyrin  B A, Tolstikhin  I N. Helium Isotopes in Nature[M]. Amsterdam:Elsevier, 1984. 175-179.
[6] Schoell M. The hydrogen and carbon isotopic composition of methane from natural gases of various origins[J]. Geochim Cosmichim Acta, 1980, 44:649-661.
[7] Schoell M. The hydrogen and carbon isotopic composition of methane from natural gases of various origins[J]. Geochemical et Cosmochimica Acta,1980, 44: 649-662.
[8] Schoell  M. Genetic characterization of natural gases[J]. AAPG Bulletin,1983, 67(12): 2225-2238.
[9] Stahl W. Carbon isotope fractionations in natural gases[J], Nature,1974, 251(5471):134-135.
[10] Stahl W. Carbon and nitrogen isotopes in hydrocarbon rese arch and exploration[J]. Chemical Geology, 1977,20: 121-149.
[11] 陈践发,徐永昌,黄第藩.塔里木盆地东部地区天然气地球化学特征及成因探讨(之一)[J]沉积学报,2000,18(4):606-609.
[12]陈践发,李春园,应光国,等. 煤型气烃类组分的稳定碳、氢同位素组成研究[J].沉积学报,1995,2:59-69.
[13]戴金星,裴锡古,戚厚发.中国天然气地质学(卷一)[M].北京:石油工业出版社,1992.114-116.
[14]戴金星.天然气碳氢同位素特征和各类天然气鉴别[J].天然气地球科学,1993,(2-3):1-40.
[15]沈平,徐永昌.中国陆相成因天然气同位素组成特征[J]地球化学,1991,(2):144-152.
[16]徐永昌,沈平,刘文汇,等.天然气中稀有气体地球化学[M]. 北京:科学出版社,1998.47-73.

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