Articles

ADVANCES IN HYDROCARBON GENERATION THEORY-(Ⅰ) IMMATURE OILS AND GENERATING HYDROCARBON AND EVOLUTIONARY MODEL

Expand
  • Research Institute of Petroleum Exploration and Development, Beijing 100083

Received date: 1995-08-21

  Revised date: 1996-02-05

  Online published: 1996-07-01

Abstract

The wide existence of immature oils throughout the world especially in China broke through the hydrocarbon generation theory through kerogen thermal degradation. Studies have shown that soluble and insoluble organic matter are organically connected in the sedimentary rock, both contributing to hydrocarbon generation. In the diagenesis,kerogen can not produce oils, so immature oils derive directly from the soluble lipids. Hydrocarbon generation process through kerogen thermal degradation takes place mainly in the early catagenesis(R o= 0.2% ~1.2%), and the oils generated are normal. In the late catagenesis, hydrocarbon generation comes into wet gas stage(R o=1.2%~2.0%), with pyrrobitumen degenerating into high mature light oils and oils cracking into gases. In this paper,the author presented a new generating hydrocarbon and evolutionary model with soluble and insoluble organic matter both contributing to the generation of hydrocarbon. 

Cite this article

Huang Difan . ADVANCES IN HYDROCARBON GENERATION THEORY-(Ⅰ) IMMATURE OILS AND GENERATING HYDROCARBON AND EVOLUTIONARY MODEL[J]. Advances in Earth Science, 1996 , 11(4) : 327 -335 . DOI: 10.11867/j.issn.1001-8166.1996.04.0327

References

[1]Philppi G T.  On the depth,  time and mechanism of petroleum generation.  Geochem Cosmochim Acta, 1965, 29:1021-1049.
[2]Louis M.  Etudes geochimiques sur les “Schistescartons”du Toarcian du Basin de Paris,  In: Advances in Organic Geochemistry 1964( eds: Hosbson G D and Louis M C)·New York: Pergamon Press, 1964. 84- 95.
[3]Louis M and Tissot B P. Influence de la temperature et de la pression sur la formation des hydrocarbures dans les argiles a kerogen. Proc Seventh World Petr Cong( Mexico),1967, 2: 47-60.
[4]Mclver R D.  Composition of Kerogen-clue to its role in the origin of petroleum.  Proc Seventh World Petr Cong(Mexico),1967, 2: 25-36.
[5]Albrecht P, Ourission G. Diagenesis des hydrocarbures satures dans une serie sedimemtaire epaisse( Douala, Cameroum).Geochem Cosmochim Acta, 1969, 33: 138- 142.
[6]Vassoevich N B, Akramkhodzhaev A M, Geodekyan A A. Principal zone of oil formation, In: Advances in Organic Geochemistry 1973(eds: Tissot B P, Bienner F).Paris: Technip, 1974. 309- 314.
[7]Tissot B P,  Welte D H.  Petroleum Formation and Occurrence.  Berling Heidelberg New York Tokyo: Spring Verlag, 1978; 1984.
[8]Hunt J M. Petroleum Geochemistry and Geology. San Francisco:  W H Freeman and Company, 1979.
[9]Lopatin N V.  The main stage of petroleum formation(in  Russian).lzv Akad Nauk Uzb SSR,  Ser Geol, 1969,1:69-76.
[10] Lopatin N V.  Temperature and geologic time factors in coalification. lzv Akad Nauk Uzb SSR, Ser Geol, 3: 95-106.
[11]Tissot B P. Primieres donnees sur lemecanismes et la cinetique de la formation du petrole dans les sediments: simulation d'un schema reactionnel sur ordinaleur. L'Inst Francais Petrol, 19, 24: 470- 501.
[12]Hood A,  Gutjaha C C M, Heacock R L. Organic metamorphism and the generation of petroleum. AAPG Bull,1975, 59: 986- 996.
[13]黄第藩,李晋超主编.中国陆相油气生成.北京:石油工业出版社,1982.
[14]黄第藩,李晋超,周翥虹,等著.陆相有机质演化和成烃机理.北京:石油工业出版社,1984. 1- 355.
[15]Snowdon L R and Powell T G. Immature oil and condensate-modification of hydrocarbon generation model for terrestrial organic matter. AAPG Bull, 1982, 66: 775-788.
[16] Palacas J G.碳酸th岩油源岩:地质和化学特征及油源对比(1983) .第11届石油会议报告论文集,第一分册(石油地质).北京:石油工业出版社,1984. 20- 34.
[17]傅家谟,盛国英,江继纲.膏岩沉积盆地形成的未熟石油.石油与天然气地质,1985, 6( 2) : 150-158.
[18]黄第藩,李晋超.陆相沉积中的未熟石油及其意义.石油学报,1987, 8(1) : 1-9.
[19]Martin R L,  Winters J C,  Willams J A, et al. Distribution of N- paraffins in crude oils and their implication to origin of petroleum. Nature, 1963, 199: 110- 113.
[20]Tannenbaum E, Aizenshtat Z. Formation of immature asphalt from organic-rich carbonate rocks一I,correlation of maturation indicates. Org Geochem, 1985, 8: 191-192.
[21]Tannenbaum E, Aizenshtat Z. Formation of immature asphalt fromorganic-rich carbonate rocks一II,correlation of maturation indicates. Org Geochem, 1984, 6: 503-511.
[22]Nissenbaum Arie,  Goldberg M,  Aizenshtat Z,  et al.  Immature condensate from Southeastern Mediterranean coastal plain, Israel. AAPG Bull, 1985, 69( 6):946- 949.
[23]史继扬,麦坎任A  S,埃格林顿G, et al.胜利油川原油和生油岩中的生物标志化合物及其应用.地球化学,1982,(1):4-19.
[24]江继纲,张谦.江汉盆地潜江期盐湖沉积石油的形成和演化.石油与天然气地质,1982, 3(1) : 1- 14.
[25]黄第藩,廖前进,徐永昌.未成熟石油成因的初步研究.中国科学院兰州地质所生物气体地球化学国家开放实验室研究年报(1987),兰州:甘肃科学技术出版社,1987. 1- 19.
[26]李茂芬,陈振岩,王延山.辽河断陷低熟油的分布及特征.见:第5届全国有机地球化学会议论文集.1992.
[27]马万怡.泌阳凹陷白云岩中未成熟原油.第二届全国有机地球化学会议论文集.
[28]黄第藩,李晋超,周翥虹,等.我国第三系陆相原油的熟化序列及其重要意义.油气资源评价研究丛书之2.北京:石油工业出版社,1989.104- 115.
[29]周光甲.陆相断块盆地中的低熟原油.第3届全国有机地球化学会议论文集.北京:地质出版社,1987.27- 37.
[30]陈建渝,何炳骏.辽东湾北部原油的类型及成因.第4届有机地球化学会议论文集.武汉:中国地质人学出版社,1990. 89-103.
[31]史继扬,汪本善,张丽洁,等.苏北盆地生油岩中苗.菇烷地球化学特征和我国东部低成熟的生油岩与原油.地球化学,1985, (1) : 80- 89.
[32]汪本善,史继扬.苏北盆地生油特征及其找油前景.地球化学论文集(1966-1986).北京:科学出版社,1986. 172-185.
[33]秦匡宗.干酪根的热解聚与未熟石油的形成.有机地球化学会议论文集.北京:地质出版社,1987.159- 168.
[34]王铁冠,钟宁宁.低熟石油的形成机理与分布.北京:石油工业出版社,1995.
[35]Laplante R E. Hydrocarbon generation in Gulf Coast Tertiary sediments. AAPG Bull,  1974, 58: 1281-1289.

Outlines

/