吐哈盆地煤成油形成的地质条件

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吐哈盆地煤成油形成的地质条件

赵长毅, 赵文智, 程克明, 牛嘉玉, 张研, 李伟

文章导航 > 沉积学报 > 1997 > 15(S1): 16-23

赵长毅, 赵文智, 程克明, 牛嘉玉, 张研, 李伟. 吐哈盆地煤成油形成的地质条件[J]. 沉积学报, 1997, 15(S1): 16-23.

引用本文:

赵长毅, 赵文智, 程克明, 牛嘉玉, 张研, 李伟. 吐哈盆地煤成油形成的地质条件[J]. 沉积学报, 1997, 15(S1): 16-23.

Zhao Changyi, Zhao Wenzhi, Cheng Keming, Niu Jiayu, Zhang Yan, Li Wei. Geological Conditions on Forming Oil-gas Field from Jurassic Coals in Tuha Basin[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 16-23.

Citation:

Zhao Changyi, Zhao Wenzhi, Cheng Keming, Niu Jiayu, Zhang Yan, Li Wei. Geological Conditions on Forming Oil-gas Field from Jurassic Coals in Tuha Basin[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 16-23.

赵长毅, 赵文智, 程克明, 牛嘉玉, 张研, 李伟. 吐哈盆地煤成油形成的地质条件[J]. 沉积学报, 1997, 15(S1): 16-23.

引用本文:

赵长毅, 赵文智, 程克明, 牛嘉玉, 张研, 李伟. 吐哈盆地煤成油形成的地质条件[J]. 沉积学报, 1997, 15(S1): 16-23.

Zhao Changyi, Zhao Wenzhi, Cheng Keming, Niu Jiayu, Zhang Yan, Li Wei. Geological Conditions on Forming Oil-gas Field from Jurassic Coals in Tuha Basin[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 16-23.

Citation:

Zhao Changyi, Zhao Wenzhi, Cheng Keming, Niu Jiayu, Zhang Yan, Li Wei. Geological Conditions on Forming Oil-gas Field from Jurassic Coals in Tuha Basin[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 16-23.

吐哈盆地煤成油形成的地质条件

石油勘探开发科学研究院

作者简介:
赵长毅,男,34岁,博士,有机岩石学和有机地球化学.

中图分类号: P618.11;P618.130.1

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文章访问数: 491
HTML全文浏览量: 9
PDF下载量: 582
被引次数: 0

Geological Conditions on Forming Oil-gas Field from Jurassic Coals in Tuha Basin

Research Institute of Petroleum Exploration and Development,CNPC,Beijing 100083

摘要: 吐哈盆地是典型的煤成油气盆地。通过对该盆地煤成油形成的地质条件分析,认为煤成油藏的形成是特定地质条件下的产物。(1)盆地构造演化控制了煤系生储油岩系发育;(2)存在低成熟成烃母质以利于烃类排出;(3)成煤沼泽氧化还原环境与成煤植物差异造成了煤原始富氢程度的不同。下三角洲平原沼泽及分流间湾沼泽是煤成烃发育的有利场所,流水沼泽相是煤成烃最有利的相带;(4)适合古地温梯度及后续盆地继承发展以保持源岩熟化,上覆湖相沉积发育以利于烃类的保存;(5)适合的构造挤压条件以利于煤成油的排驱与运移。
- 吐哈盆地 /
- 煤成油 /
- 形成条件 /
- 油气藏
Abstract: The Tuha basin is a typical coal-derived oil-gas basin. Through analyzing the geological and geochemical conditions formingcoal-derived oil in this basin, the coal-derived oil pool is rnnsidered to be formed under a specially designated geological condition.(1) The development of source rocks and reservoir of coal measures is controlled by the tectonic evolution of basin. (2) Low-ma-lure source materials are favorable for the expulsion of h州rocarbons. ( 3 ) Redox environments of coal-forming swamp and coal-forming plants result in the difference of hydrogen-rich degree in coal. Lower delta plain and interdistributary bay swamps are fa-vorable for the development of coal-derived hydrocarbon, and running water swamp facies is the most favorable facies zone for hy-drocarbon generation from coal. (4) Appropriate paleogeothermal gradient and inherited development of basin is advantageous tomaturation of source rock, and the development of overlying lake deposit is beneficial to the preservation of the expulsive hydrocar-boas from coalbed. (5) Suitable tectonic compressing is favorable for the expulsion and migration of coal-derived oil.
- Tuha basin /
- Coal-derived oil /
- formation crondition /
- oil-gas pool

参考文献(13)

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[2]	Brooks J. D. and Smith J. W.，The diagenesis of plant lipids dur-ing the formation of coal, petroleum and natural gas-I.Changes in the n-paraffin hydrocarbons. Geochim. Cosmochim.Acta. 1967, 31:289-297.
[3]	Brooks J.D. and Smith J. W.. The diagenesis of plant lipids dur-ing the formation of coal, petroleum and natural gas-1(.Coalifi-canon and the formation of oil and gas in the Gippsland Basin.Geochim. Cosmochim. Acta. 1967, 33:1183-1194.
[4]	Rigby D. and Smith J. W.，An isotopic study of gases and hydro-carbons in the Cooper Basin. APEA Journal. 1981, 21(1) : 222-229.
[5]	Durand B. and Paratte M.，Oil potential of coals: a geochemicalapproach, In Petroleum Geochemistry and Exploration of Europe( Edited By Brooks J. and Welte D. H.)，Blackwell Oxford.1983, 255 - 265.
[6]	Snowdon L. R. and Powell T. G..Immature oil and mndensate is matter, AAPG. Bull，1982, 66(6):775-778.
[7]	Pilaar W. F. H. and Wakefield L. L.，Hydrocarbon generation inthe Taranaki Basin, New Zealand405-424. memoir 35, 1984
[8]	Evamy B. D.，Haremboure J.，Kamerling P.，Knapp W . A.， Molloy F. A. and Rowlands P. H.，Hydrocarbon habitat of Ter- nary Niger Delta. AAPG. 1978. 62:1-37.
[9]	Hvaslef S.，Larter S. R. and Leythaeuser. Aspects of generation and migration of hydrocarbons from coal-bearing strata of the Hi- tra formation, Haltenbanken area, offsore Norway, Advances in Organic Geochemistry, 1987, 525-536.
[10]	Clayton 1. L.，Rice D. D. and Michael G. E.,Oil-generating coals of the San Juan Basin, New Mexico and Colorado, U. S. A.，Organic Geochemistry, 1991, 17(6):735-742.
[11]	中国煤田地质总局.中国煤岩学图鉴.北京:中国矿业大学出版社，1996
[12]	赵长毅等.吐哈盆地煤中基质镜质体生烃潜力与特征科学通报，1994,39(21);1979-1981
[13]	杨起，韩德馨。中国煤田地质学(上册).北京:煤炭工业出版社，1979 [14〕杨起主编.煤地质学进展.北京:科学出版社.1987.

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计量

文章访问数: 491
HTML全文浏览量: 9
PDF下载量: 582
被引次数: 0

吐哈盆地煤成油形成的地质条件

石油勘探开发科学研究院

作者简介:
赵长毅,男,34岁,博士,有机岩石学和有机地球化学.

收稿日期: 1996-12-30
刊出日期: 1997-12-31

中图分类号: P618.11;P618.130.1

关键词:

摘要: 吐哈盆地是典型的煤成油气盆地。通过对该盆地煤成油形成的地质条件分析,认为煤成油藏的形成是特定地质条件下的产物。(1)盆地构造演化控制了煤系生储油岩系发育;(2)存在低成熟成烃母质以利于烃类排出;(3)成煤沼泽氧化还原环境与成煤植物差异造成了煤原始富氢程度的不同。下三角洲平原沼泽及分流间湾沼泽是煤成烃发育的有利场所,流水沼泽相是煤成烃最有利的相带;(4)适合古地温梯度及后续盆地继承发展以保持源岩熟化,上覆湖相沉积发育以利于烃类的保存;(5)适合的构造挤压条件以利于煤成油的排驱与运移。

English Abstract

赵长毅, 赵文智, 程克明, 牛嘉玉, 张研, 李伟. 吐哈盆地煤成油形成的地质条件[J]. 沉积学报, 1997, 15(S1): 16-23.

引用本文:

赵长毅, 赵文智, 程克明, 牛嘉玉, 张研, 李伟. 吐哈盆地煤成油形成的地质条件[J]. 沉积学报, 1997, 15(S1): 16-23.

Zhao Changyi, Zhao Wenzhi, Cheng Keming, Niu Jiayu, Zhang Yan, Li Wei. Geological Conditions on Forming Oil-gas Field from Jurassic Coals in Tuha Basin[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 16-23.

Citation:

Zhao Changyi, Zhao Wenzhi, Cheng Keming, Niu Jiayu, Zhang Yan, Li Wei. Geological Conditions on Forming Oil-gas Field from Jurassic Coals in Tuha Basin[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 16-23.

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