| 陆相沉积盆地指相生物标记物及分子参数 |
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| 引用本文： | 尚慧芸,姜乃煌.陆相沉积盆地指相生物标记物及分子参数[J].沉积学报,1983,1(1):107-117. |
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| 作者姓名： | 尚慧芸 姜乃煌 |
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| 作者单位： | 石油工业部北京石油勘探开发研究院 |
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| 摘 要： | 沉积相是在特定环境条件下形成的地质体,沉积相的研究.在石油地质研究中占有重要地位。根据国内外油气勘探表明,油气的生成与分布.均与沉积相带有密切的关系1]。我国陆相沉积盆地,与海相沉积盆地相比较,具有多物源,多沉积体系,相带多呈环状公布的特征。勘探实践及研究表明,沉积相带的分布与油气生成及聚集关系密切。
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| 收稿时间： | 1982-05-28 |
SEDIMENTARY FACIES INDICATORS OF BIOMARKERS AND THEIR MOLECULAR PARAMETERS IN TERRESTRIAL BASINS |
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| Institution: | Scientific Research Institute of Petroleum Exploration and Development, Beijing |
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| Abstract: | Sedimentary facies is the major control of petroleum origin, migration and distribution in terrestrial basins.The common study methods of sedimentary facies are based on the characteristics of sedimentary sequence and various markers such as rock facies, mineral facies, biological fossils, trace fossils, rock structure, etc.and they are classified by geochemical indicators.We have used GC-MS to analyze the samples of different sedimentary facies (swamp facies, littoral and shallow water lacustrine facies, subdeep-deep water lacustrine facies) of triterpanes and steranes in an attempt to find out the sedimentary facies indicators of biomarkers and their molecular parameters in terrestrial basins Sedimentary facies indicator of biomarkers is one of the means of measarement to study sedimentary facies on molecular level and it is also a complemental means to the conventional methods.In geological period,the biomarker compounds had more stable carbon skeleton, they transferred the informations of primary living organisms, and were closely related to biological bodies.The study of sedimentary facies of terrestrial basin shows that the type of organic matter in source rocks is controlled on the plane by the belts of the sedimentary facies.Land plants are mostly distributed on the lakeshore, whereas aquatic organisms at the central part of the lake.Therefore, the biomarkcrs used to recognize the type of organic matter and their molecular parameters may also be used as compounds of facies indicators of biomarkers. Different facies from lower Cretaceous Qingshankon 2-3 member of Songliao basin, and samples of different ages but in the same sedimentary facies from Pale-agene Shahejie formation of Bohai Bay basin, lower Cretaceous Qingshankon 2-3 member of Songliao basin, Jurassic Yunan formation of Erduosi basin have been analyzed by comparing and examining triterpanes and steranes from different sedimentary facies along with geological and geochemical data, and therefore we have got some knowledge about sedimentary facies indicators of biomarkers of the terrestrial basin. Based on the study of biomarker in sedimentary facies belts from the basins,we have suggested that oleanane, C29-hopane/C30-hopane, Tm/TS,ΣC27 + C29-hopane/Σ C30-hopanes andΣC27-steranes/Σ C29-steranes, 4 -methyl-C29-steranes/5α-C27-ster-anes can be used as indicators of the biomarkers and molecular parameters. By using geochemical parameters, the sedimentary facies bands may be classified as follows: The swamp facies,in general,contain oleanane and C29-hopane/C30-hopane, Tm/TS, Σ C27+C29/Σ C30 are higher, while in steranes Σ C27/Σ C29 is relatively lower but the 4 -methyl-C29/5α-C27 higher.The characteristics of subdeep-deep lacustrine facies is contrary to the previous discussion.The lakeshore facies are moderate in characteristics of the two mentioned above. The authors believe that better results can be acheivcd if facies indicators of biomarkers and their molecular parameters are used to classify the sedimentary facies in company with geological and geochemical parameters.The biomarkers and their parameters suggested in this paper have shown their applicability to the samples studied. |
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