天然气地球化学

柴北缘马海地区油气全烃地球化学特征与成因

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  • 1.西南石油学院,四川 成都  610500;2.中国石油青海油田分公司勘探开发研究院,甘肃  敦煌 736202
胡雄(1972-),男,四川绵竹人,助教,硕士,主要从事油气地球化学研究.

收稿日期: 2005-04-14

  修回日期: 2005-07-14

  网络出版日期: 2005-10-20

ORIGIN AND WHOLE-HYDROCARBON GEOCHEMICAL CHARACTISTICS OF OIL AND GAS FROM MAHAI AREA,NORTH EDGE OF QAIDAM BASIN

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  • 1.Southwest Petroleum Institute, Chendu  610500, China;  2.Research Institute of Exploration and Development of Qinghai Oil Field Branch Company, Dunhuang  736202,China

Received date: 2005-04-14

  Revised date: 2005-07-14

  Online published: 2005-10-20

摘要

通过对天然气组成、油气碳同位素、原油轻烃、中分子量烃和生物标志化合物等的研究,阐明了柴北缘马海地区油气的全烃地球化学特征,区分了不同油气的成因类型和可能来源。指出南八仙油气田和马海气田天然气为同一成因类型,南八仙油气田天然气属于高-过成熟煤成气,与伊北凹陷下侏罗统煤系烃源岩有关,而马北构造主要为高成熟早期腐殖型有机质成因为主的湿气,与尕丘凹陷和尕西次凹侏罗系腐殖型烃源岩有关;南八仙油气田原油主要属于煤成油,马北构造油则主要属于混合偏腐泥型成因油。

本文引用格式

胡雄;李延钧;陈新领;江波;马立协;付晓文;王强;梁艳; . 柴北缘马海地区油气全烃地球化学特征与成因[J]. 天然气地球科学, 2005 , 16(5) : 612 -616 . DOI: 10.11764/j.issn.1672-1926.2005.05.612

Abstract

The paper adopts some methods such as gas composition, light hydrocarbon,carbon isotope,middle-molecular hydrocarbon and biomarker to illustrate whole-hydrocarbon geochemical charactistics of oil and gas from Mahai area and identify the genetictype and source of the different genetic oil.  The result shows that gas from Nanbaxian and Mabei oil-gas field is the same genetic type, But the gas of Nanbaxian field is mainly high-over mature coal formed gas ,which is associated with lower Jurassic coal source rock in Yibei depression. Natural gas from Mabei structure is mainly wet gas of high mature early period, which is associate with Jurassic humic source rock in Gaqiu depression and Gaxi hypo-depression.  Crude oil is mainly coal formed oil in Nanbaxian field, while crude oil is mainly sapropel-type oil in Mabei structure.

参考文献

   [1] 文志刚, 王正允, 何幼斌, 等.柴达木盆地北缘上石炭统烃源岩评价[J].天然气地球科学,2004,15(2):125-127.
[2] 彭立才,刘兰桂.柴达木盆地北缘侏罗系烃源岩沉积有机相划分及评价[J].石油与天然气地质,2001,22(2):178-181.
[3] 戴金星.天然气地质学概论[M].北京:石油工业出版社.1999.
[4] 戴金星,秦胜飞,陶士振,等.中国天然气工业发展趋势和天然气地学理论重要进展[J].天然气地球科学,2005,16(2):127-142.
[5] 徐永昌.天然气的成因理论及应用[M].北京:科学出版社,1994.
[6] 徐永昌.天然气地球化学研究及有关问题探讨[J].天然气地球科学,1999,10(3):20-28.
[7] Littk R, Kroos B. Molecular nitrogen in natural gas accumulations:Generation from sedimentary organic matter at high temperatures[J].AAPG,1995,79(3):410.
[8] Hunt J H. 石油地球化学与地质学[M].北京:石油工业出版社,1979.
[9] 张同伟,王先彬.鄂尔多斯盆地酸解烃碳同位素组成与气-源对比[J].科学通报,1996,41(3):242-244.
[10] 傅家谟,刘德汉,盛国英,等.煤成烃地球化学.北京:科学出版社,1990.306-307.
[11] 陈建平,赵长毅,王兆云,等. 西北地区侏罗系烃源岩及原油地球化学特征[J].地质论评,1998,44(2):49-59.
[12] 张义纲.天然气的生成聚集和保存.南京:河海大学出版社,1991.59-61.
[13] Chung H.Moses .Mixed signals of the source and thermal maturity for petroleum accumulations from light hydrocarbons:an example of the Beryl field. OrgGeochem,1998,29:381-396
[14] Hwang R J. Oil composition variation and reservoir continuity: Unity Field Sudan[J].Org Geochem,1994,21(2):171-188.

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