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Wang Kaifa, Wu Guoxuan, Yan Jialin. ON SPORO-POLLEN COLOR AND ORGANIC MATTER TYPES OF LOWER TERTIARY IN BIYANG AND ZAOYANG DEPRESSIONS,NANXIANG BASIN[J]. Acta Sedimentologica Sinica, 1984, 2(3): 108-117.
Citation: Wang Kaifa, Wu Guoxuan, Yan Jialin. ON SPORO-POLLEN COLOR AND ORGANIC MATTER TYPES OF LOWER TERTIARY IN BIYANG AND ZAOYANG DEPRESSIONS,NANXIANG BASIN[J]. Acta Sedimentologica Sinica, 1984, 2(3): 108-117.

ON SPORO-POLLEN COLOR AND ORGANIC MATTER TYPES OF LOWER TERTIARY IN BIYANG AND ZAOYANG DEPRESSIONS,NANXIANG BASIN

  • Received Date: 1983-05-18
  • Publish Date: 1984-09-10
  • This paper deals with the visual observation of sporo-pollen color and organic matter types of the 4 wells of the Biyang aad Zaoyang depressions (a total of 57 samples). All of the samples were treated with hydrochloric and hydrofluoric acids to remove carbonates and silicates, then the organic materials contained in them were concentrated by means of heavy liquid ( CdI2 ). Sporo-pollen fossils and other organic matters were observed under transmission microscope. Based on the variations of sporo-pollen color, three organic maturation facies may be distinguished: ( i ) the light yellow and yellow are immature, ( ii ) the yellowish-brown and brown indicate mature to highly mature, and ( iii ) the dark brownish-black and black are metamorphosed. Dry gas and possibly heavy oil could be generated in the immature facies; oil, condensate and wet gas could be found in the mature to highly mature facies; only dry gas could be produced in the metamorphosed facies. Three main types of organic matters in sedimentary rocks can be determined under transmission micros-cope, e.g. sapropel type,humus type and transitional type. In the mature to highly mature facies, the sapropel type and transitional type produce oil, condensate and wet gas,
  • [1] (1)朱水安,徐世荣等,1981,河南泌阳凹陷的石油地质特征,石油学报,第2卷2期。

    (2)西北大学地质系石油地质教研室,1979,石油地质学,地质出版社。

    (3)B, P、蒂索,D. H、威尔特、石油形成和分布—油气勘探新途径.郝石生等译,1982.石油工业出版让.

    (4)J, M, Hunt, 1919, Petroleum Geochemis-trv and Geology. W. H. Freeman and Company San Francisco.

    (5)F, L, Staplin, 1969, Sedimentary Organic Matter, Organic Metamorphism and Oil and Gas Occurrence, Bull, Canadian Petroleum GeologyV.17, No.1, 47一66

    (6)B. Durand, 1980, Kerogen一insoluble Organic Mattcr from Sedimentary Rocks,Techip一Paris,
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  • Received:  1983-05-18
  • Published:  1984-09-10

ON SPORO-POLLEN COLOR AND ORGANIC MATTER TYPES OF LOWER TERTIARY IN BIYANG AND ZAOYANG DEPRESSIONS,NANXIANG BASIN

Abstract: This paper deals with the visual observation of sporo-pollen color and organic matter types of the 4 wells of the Biyang aad Zaoyang depressions (a total of 57 samples). All of the samples were treated with hydrochloric and hydrofluoric acids to remove carbonates and silicates, then the organic materials contained in them were concentrated by means of heavy liquid ( CdI2 ). Sporo-pollen fossils and other organic matters were observed under transmission microscope. Based on the variations of sporo-pollen color, three organic maturation facies may be distinguished: ( i ) the light yellow and yellow are immature, ( ii ) the yellowish-brown and brown indicate mature to highly mature, and ( iii ) the dark brownish-black and black are metamorphosed. Dry gas and possibly heavy oil could be generated in the immature facies; oil, condensate and wet gas could be found in the mature to highly mature facies; only dry gas could be produced in the metamorphosed facies. Three main types of organic matters in sedimentary rocks can be determined under transmission micros-cope, e.g. sapropel type,humus type and transitional type. In the mature to highly mature facies, the sapropel type and transitional type produce oil, condensate and wet gas,

Wang Kaifa, Wu Guoxuan, Yan Jialin. ON SPORO-POLLEN COLOR AND ORGANIC MATTER TYPES OF LOWER TERTIARY IN BIYANG AND ZAOYANG DEPRESSIONS,NANXIANG BASIN[J]. Acta Sedimentologica Sinica, 1984, 2(3): 108-117.
Citation: Wang Kaifa, Wu Guoxuan, Yan Jialin. ON SPORO-POLLEN COLOR AND ORGANIC MATTER TYPES OF LOWER TERTIARY IN BIYANG AND ZAOYANG DEPRESSIONS,NANXIANG BASIN[J]. Acta Sedimentologica Sinica, 1984, 2(3): 108-117.
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