Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression

ZHU Guang-you; JIN Qiang

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Article Navigation > Acta Sedimentologica Sinica > 2003 > 21(3): 506-512

ZHU Guang-you, JIN Qiang. Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression[J]. Acta Sedimentologica Sinica, 2003, 21(3): 506-512.

Citation:

ZHU Guang-you, JIN Qiang. Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression[J]. Acta Sedimentologica Sinica, 2003, 21(3): 506-512.

Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression

College of Geo-Resource and Information,University of Petroleum,Dongying Shan dong 257061

Received Date: 2002-08-27
Rev Recd Date: 2002-11-08
Publish Date: 2003-09-10

Abstract

The crude oil in Dongying depression mainly came from underlayer of Member 3 and upperlayer of Member 4 source rocks in the Shahejie Formation. On the basis of abundant geochemical data, the authors analyzed the discrepancies in sedimen ta ry and geochemical characteristics of the two sets of source rocks. The underlay er of Member 3 developed in deep lake-semideep lake with saline water-semisal ine water, but the upperlayer of Member 4 formed in shallow lake-semideep lake wi th brine water-saline water. Moreover, the authors discussed the accumulatio n and preservation features of organic matter and pointed out that high paleo-pro duct ivity and anoxic environment controlled the formation of the two sets of excelle nt source rocks. Brine condition has an important effect on upperlayer of Membe r 4 and algal blooms controlled the formation of source rocks with rich organic m atter in upperlayer of Member 4 and underlayer of member 3.
- excellent source rock,
- Dongying depression,
- Shahejie Formation,
- anoxic environment,
- paleo- productivity

References

[1]	郭元岭,赵乐强,石红霞等.济阳坳陷探明石油地质储量特点分析[J].石油勘探与开发,2001, 28(3):33～37[Guo Yuanling, Zhao Leqing, Shi Hongxia, et al. Analys is on characteristic of proven OOIP in Jiyang depression[J]. Petroleum Exploration and Development, 2001,28(3):33～37]
[2]	曾溅辉,郑和荣,王宁.东营凹陷岩性油气藏成藏动力学特征[J].石油与天然气地质,1998,19(4):326～329[Zeng Jianhui, Zheng Herong, Wang Ning. Pool-forming dynamic property of lithological oil-gas reservoirs in Dingying sag[J]. Oil & Gas Geology, 1998,19(4):326～329]
[3]	金强.有效烃源岩的重要性及其研究[J].油气地质与采收率, 2001,8(1):1～4[Jin Qiang. Importance and research about effective hydrocarbon source rock[J]. Petroleum Geology and Recovery Efficiency, 2001, 8(1):1～4]
[4]	金强,查明.柴达木盆地西部第三系蒸发岩与生油岩共生沉积作用研究[J].地质科学, 2000,35(4):465～473[Jin Qiang, Zha Ming. Co-sedimentation of Tertiary evaporates and oil source rocks in the western Qaidam basin[J]. Scientia Geologica Sinica, 2000,35(4):465～473]
[5]	张水昌,张保民,王飞宇等.塔里木盆地两套海相有效烃源岩层-Ⅰ有机质性质、发育环境及控制因素[J].自然科学进展,2001,11(3):261～268[Zhang Shuichang,Zhang Baomin,Wang Feiyu,et al.The two sets of effective source rock layers in Talimu Basin-Ⅰ the organic matters characteristics, developing environment and controlling factors[J]. Progress in Nature Science, 2001,11(3):261～268]
[6]	孔凡仙,张林晔,周文等.济阳坳陷优质烃源岩层地球化学特征及成烃潜力[J].复式油气田,2000,7(3):13～15[Kong Fanxian, Zhang Linye, Zhou Wen, et al.Geochemical characteristics and hydrocarbon-generating potential of good source rocks in Jiyang depression[J]. Multiple Oil-Gas Field, 2000, 7(3):13～15]
[7]	李成风,肖继风.用微量元素研究胜利油田东营盆地沙河街组的古盐度[J].沉积学报,1988,6(4):100～107[Li Chengfeng, Xiao Jifeng. The application of trace element to the study on paleosalinities in Shahejie Formation of Dongying basin, Shengli oil field[J]. Acta Sedimentologica Sinica, 1988,6(4):100～107]
[8]	朱光有,金强.烃源岩的非均质性及其研究-以东营凹陷牛38井为例[J].石油学报,2002,23(4):34～39[Zhu Guangyou,Jin Qiang. On Source rock heterogeneity-A case study of the Well Niu-38, Dongying Depression[J]. Acta Petrolei Sinica, 2002, 23(4):34～39]
[9]	Seifert W K, Moldowan J M. The effect of biodegradation on steranes and terpanes in crude oils[J]. Geochimica et Coschimica Acta, 1979,43:111～126
[10]	Seifert W K, Moldowan J M. Paleoreconstruction by biological markers[J]. Geochimica et Coschimica Acta, 1981,45:783～794
[11]	李任伟,林大兴,王志珍等.判断高盐度环境的新标准[J].科学通报,1986,(8):604～607[Li Renwei,Lin Daxing,Wang Zhizhen,et al.The new criteria used by judging high-salinity environment[J]. Chinese Science Bulletin, 1986,(8):604～607]
[12]	王铁冠.试论我国某些原油与生油岩中的沉积环境标志物[J].地球化学,1990,(3):256～262[Wang Tieguan. A contribution to some sedimentary environmental biomarkers in crude oils and source rocks in China[J]. Geochimica, 1990,3:256～262]
[13]	傅家谟,盛国英,许家友等.应用生物标志化合物参数判别古沉积环境[J].地球化学,1991,(1):1～12[Fu Jiamo,Sheng Guoying, Xu Jiayou, et al. Application of biomarker compounds in assessment of paleoenvironments of Chinese terrestrial sediments[J]. Geochimica, 1991,(1):1～12]
[14]	张枝焕,杨藩,李东明等.中国新生界咸化湖相烃源岩和原油生物标志物组合特征[J].沉积学报,1998,16(3):119～123[Zhang Zhihuan, Yang Fan, Li Dongming, et al. Biomarker assemblage characteristics of source rocks and associated crude oil in saline lake facies of Cenozoic in China[J]. Acta Sedimentologica Sinica, 1998,16(3):119～123]
[15]	唐祥华.东濮凹陷早第三纪钙质超微化石古生态及成盐环境[J].科学通报,1986,(4):298～300[Tang Xianghua.The Palaeogene super-micro fossil palaeoecology and haloenvironment in Dongpu depression[J].Chinese Science Bulletin, 1986,(4):298～300]
[16]	李春光.论山东东营、惠民盆地油田水与油气聚集关系[J].地质论评,1994,40(4):340～346[Li Chunguang. The relationship between oil-field water and hydrocarbon accumulation in the Dongying and Huimin basins, Shandong[J]. Geological Review, 1994,40(4):340～346]
[17]	裘松余,卢兵力.我国东部晚白垩世和早第三纪海侵与油气关系[J].地质论评,1994,40(3):229～235[Qiu Songyu, Lu Bingli. The relationship of late Cretaceous and early Tertiary transgressins to hydrocarbons in eastern China[J]. Geological Review, 1994, 40(4):340～346]
[18]	侯读杰,王铁冠.陆相湖盆沉积物和原油中的甲藻甾烷[J].科学通报,1995,40(4):333～335[Hou Dujie,Wang Tieguan. The sediment in continental lacustrine basin dinosterane in crude oil[J].Chinese Science Bulletin, 1995,40(4):333～335]
[19]	姚益民,徐金鲤,单怀广等.山东济阳坳陷早第三纪海侵的讨论[J].石油学报,1992,13(2):29～34[Yao Yimin, Xu Jinli, Shan Huaiguang, et al. A discussion of the paleogene transgression in the Jiyang depression, Shandong province[J]. Acta Petrolei Sinica. 1992,13(2):29～34]
[20]	陈致林,李素娟.甲藻甾烷一种物源和沉积环境的生物标志物[J].石油勘探与开发,1994, 21(3):60～64[Cheng Zhilin, Li Sujuan. Dinosterane as biomarker of biogenic origin and sedimentary environment[J]. Petroleum Exploration and Development, 1994,21(3):60～64]
[21]	刘传联,成鑫荣.渤海湾盆地早第三纪非海相钙质超微化石的锶同位素证据[J].科学通报,1996,41(10):908～910[Liu Chuanlian, Cheng Xinrong. Strontium isotopic evidences of the Eocene non-marine calcareous ultra-micro-fossils in Bohai Bay basin[J]. Chinese Science Bulletin, 1996,41(10):908～910]
[22]	李守军.渤海湾盆地早第三纪水平面升降和全球海平面升降的不一致性[J].地质论评,1998,44(1):31～34[Li Shujun. Inconsistency between water-level change in the Bohai bay basin and eustasy during the paleogene[J]. Geological Review, 1998,44(1):31～34]
[23]	Pederson T F and Calvert S E. Anoxia versus productivity:what controls the formation of organic-carbon-rich sediments and sedimentary rock? [J]. AAPG Bulletin, 1990,74:454～466
[24]	刘传联,徐金鲤,汪品先.藻类勃发-湖相油源岩形成的一种重要机制[J].地质论评, 2001,47(2):207～209[Liu Chuanlian, Xu Jinli, Wang Pinxian. Algal blooms: the primary mechanism in the formation of lacustrine petroleum source rocks[J].Geological Review, 2001,47(2):207～210]
[25]	Ribouleau A, Derenne S, Largeau C. Origin of contrasting features and preservation pathways in kerogens from the Kashpir oil shales(Upper Jurassic, Russian Platform) [J]. Organic Geochemistry, 2001, 32(5):647～665
[26]	Dahl J E P, Moldowman J M, Teerman S C. Source rock quality determination from oil biomarkers I: a new geochemical technique[J]. AAPG Bulletin, 1994,78(10):1 507～1 526
[27]	Harrison S P,Digerfeldt G. European lake as palaeohydrological and palaeoclimatic indicators[J]. Quaternary Science Review, 1993,12:233～248
[28]	Peters K E, Moldowan J M. The biomarker guide-Interpreting molecular fossils in petroleum and ancient sediments[M]. Prentice Hall, New Jersey. 1993,88
[29]	张立平,黄第藩,廖志勤.伽马蜡烷-水体分层的地球化学标志[J].沉积学报,1999,17(1):136～140[Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerance - geochemical indicator of water column stratification[J]. Acta Sedimentologica Sinica, 1999,17(1):136～140]
[30]	王铁冠.论分子有机地球化学若干名词与术语的辨析和厘定[J].地质论评, 2002,48(3):284～289[Wang Tieguan. Discrimination and stipulation of some terms of molecular organic geochemistry[J]. Geological Review, 2002, 48(3):284～289]
[31]	王慧中,梅洪明.东营凹陷沙三下亚段油页岩中古湖泊学信息[J].同济大学学报,1998,26(3):315～319[Wang Huizhong, Mei Hongming. Paleolimnological information from the oil shale in the lower part of Sha 3 Formation, in Dongying depression[J]. Journal of Tongji University, 1998, 26(3):315～319]

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Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression

College of Geo-Resource and Information,University of Petroleum,Dongying Shan dong 257061

Received Date: 2002-08-27

Rev Recd Date: 2002-11-08

Publish Date: 2003-09-10

Key words:

Abstract: The crude oil in Dongying depression mainly came from underlayer of Member 3 and upperlayer of Member 4 source rocks in the Shahejie Formation. On the basis of abundant geochemical data, the authors analyzed the discrepancies in sedimen ta ry and geochemical characteristics of the two sets of source rocks. The underlay er of Member 3 developed in deep lake-semideep lake with saline water-semisal ine water, but the upperlayer of Member 4 formed in shallow lake-semideep lake wi th brine water-saline water. Moreover, the authors discussed the accumulatio n and preservation features of organic matter and pointed out that high paleo-pro duct ivity and anoxic environment controlled the formation of the two sets of excelle nt source rocks. Brine condition has an important effect on upperlayer of Membe r 4 and algal blooms controlled the formation of source rocks with rich organic m atter in upperlayer of Member 4 and underlayer of member 3.

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Reference (31)

[1]	郭元岭,赵乐强,石红霞等.济阳坳陷探明石油地质储量特点分析[J].石油勘探与开发,2001, 28(3):33～37[Guo Yuanling, Zhao Leqing, Shi Hongxia, et al. Analys is on characteristic of proven OOIP in Jiyang depression[J]. Petroleum Exploration and Development, 2001,28(3):33～37]
[2]	曾溅辉,郑和荣,王宁.东营凹陷岩性油气藏成藏动力学特征[J].石油与天然气地质,1998,19(4):326～329[Zeng Jianhui, Zheng Herong, Wang Ning. Pool-forming dynamic property of lithological oil-gas reservoirs in Dingying sag[J]. Oil & Gas Geology, 1998,19(4):326～329]
[3]	金强.有效烃源岩的重要性及其研究[J].油气地质与采收率, 2001,8(1):1～4[Jin Qiang. Importance and research about effective hydrocarbon source rock[J]. Petroleum Geology and Recovery Efficiency, 2001, 8(1):1～4]
[4]	金强,查明.柴达木盆地西部第三系蒸发岩与生油岩共生沉积作用研究[J].地质科学, 2000,35(4):465～473[Jin Qiang, Zha Ming. Co-sedimentation of Tertiary evaporates and oil source rocks in the western Qaidam basin[J]. Scientia Geologica Sinica, 2000,35(4):465～473]
[5]	张水昌,张保民,王飞宇等.塔里木盆地两套海相有效烃源岩层-Ⅰ有机质性质、发育环境及控制因素[J].自然科学进展,2001,11(3):261～268[Zhang Shuichang,Zhang Baomin,Wang Feiyu,et al.The two sets of effective source rock layers in Talimu Basin-Ⅰ the organic matters characteristics, developing environment and controlling factors[J]. Progress in Nature Science, 2001,11(3):261～268]
[6]	孔凡仙,张林晔,周文等.济阳坳陷优质烃源岩层地球化学特征及成烃潜力[J].复式油气田,2000,7(3):13～15[Kong Fanxian, Zhang Linye, Zhou Wen, et al.Geochemical characteristics and hydrocarbon-generating potential of good source rocks in Jiyang depression[J]. Multiple Oil-Gas Field, 2000, 7(3):13～15]
[7]	李成风,肖继风.用微量元素研究胜利油田东营盆地沙河街组的古盐度[J].沉积学报,1988,6(4):100～107[Li Chengfeng, Xiao Jifeng. The application of trace element to the study on paleosalinities in Shahejie Formation of Dongying basin, Shengli oil field[J]. Acta Sedimentologica Sinica, 1988,6(4):100～107]
[8]	朱光有,金强.烃源岩的非均质性及其研究-以东营凹陷牛38井为例[J].石油学报,2002,23(4):34～39[Zhu Guangyou,Jin Qiang. On Source rock heterogeneity-A case study of the Well Niu-38, Dongying Depression[J]. Acta Petrolei Sinica, 2002, 23(4):34～39]
[9]	Seifert W K, Moldowan J M. The effect of biodegradation on steranes and terpanes in crude oils[J]. Geochimica et Coschimica Acta, 1979,43:111～126
[10]	Seifert W K, Moldowan J M. Paleoreconstruction by biological markers[J]. Geochimica et Coschimica Acta, 1981,45:783～794
[11]	李任伟,林大兴,王志珍等.判断高盐度环境的新标准[J].科学通报,1986,(8):604～607[Li Renwei,Lin Daxing,Wang Zhizhen,et al.The new criteria used by judging high-salinity environment[J]. Chinese Science Bulletin, 1986,(8):604～607]
[12]	王铁冠.试论我国某些原油与生油岩中的沉积环境标志物[J].地球化学,1990,(3):256～262[Wang Tieguan. A contribution to some sedimentary environmental biomarkers in crude oils and source rocks in China[J]. Geochimica, 1990,3:256～262]
[13]	傅家谟,盛国英,许家友等.应用生物标志化合物参数判别古沉积环境[J].地球化学,1991,(1):1～12[Fu Jiamo,Sheng Guoying, Xu Jiayou, et al. Application of biomarker compounds in assessment of paleoenvironments of Chinese terrestrial sediments[J]. Geochimica, 1991,(1):1～12]
[14]	张枝焕,杨藩,李东明等.中国新生界咸化湖相烃源岩和原油生物标志物组合特征[J].沉积学报,1998,16(3):119～123[Zhang Zhihuan, Yang Fan, Li Dongming, et al. Biomarker assemblage characteristics of source rocks and associated crude oil in saline lake facies of Cenozoic in China[J]. Acta Sedimentologica Sinica, 1998,16(3):119～123]
[15]	唐祥华.东濮凹陷早第三纪钙质超微化石古生态及成盐环境[J].科学通报,1986,(4):298～300[Tang Xianghua.The Palaeogene super-micro fossil palaeoecology and haloenvironment in Dongpu depression[J].Chinese Science Bulletin, 1986,(4):298～300]
[16]	李春光.论山东东营、惠民盆地油田水与油气聚集关系[J].地质论评,1994,40(4):340～346[Li Chunguang. The relationship between oil-field water and hydrocarbon accumulation in the Dongying and Huimin basins, Shandong[J]. Geological Review, 1994,40(4):340～346]
[17]	裘松余,卢兵力.我国东部晚白垩世和早第三纪海侵与油气关系[J].地质论评,1994,40(3):229～235[Qiu Songyu, Lu Bingli. The relationship of late Cretaceous and early Tertiary transgressins to hydrocarbons in eastern China[J]. Geological Review, 1994, 40(4):340～346]
[18]	侯读杰,王铁冠.陆相湖盆沉积物和原油中的甲藻甾烷[J].科学通报,1995,40(4):333～335[Hou Dujie,Wang Tieguan. The sediment in continental lacustrine basin dinosterane in crude oil[J].Chinese Science Bulletin, 1995,40(4):333～335]
[19]	姚益民,徐金鲤,单怀广等.山东济阳坳陷早第三纪海侵的讨论[J].石油学报,1992,13(2):29～34[Yao Yimin, Xu Jinli, Shan Huaiguang, et al. A discussion of the paleogene transgression in the Jiyang depression, Shandong province[J]. Acta Petrolei Sinica. 1992,13(2):29～34]
[20]	陈致林,李素娟.甲藻甾烷一种物源和沉积环境的生物标志物[J].石油勘探与开发,1994, 21(3):60～64[Cheng Zhilin, Li Sujuan. Dinosterane as biomarker of biogenic origin and sedimentary environment[J]. Petroleum Exploration and Development, 1994,21(3):60～64]
[21]	刘传联,成鑫荣.渤海湾盆地早第三纪非海相钙质超微化石的锶同位素证据[J].科学通报,1996,41(10):908～910[Liu Chuanlian, Cheng Xinrong. Strontium isotopic evidences of the Eocene non-marine calcareous ultra-micro-fossils in Bohai Bay basin[J]. Chinese Science Bulletin, 1996,41(10):908～910]
[22]	李守军.渤海湾盆地早第三纪水平面升降和全球海平面升降的不一致性[J].地质论评,1998,44(1):31～34[Li Shujun. Inconsistency between water-level change in the Bohai bay basin and eustasy during the paleogene[J]. Geological Review, 1998,44(1):31～34]
[23]	Pederson T F and Calvert S E. Anoxia versus productivity:what controls the formation of organic-carbon-rich sediments and sedimentary rock? [J]. AAPG Bulletin, 1990,74:454～466
[24]	刘传联,徐金鲤,汪品先.藻类勃发-湖相油源岩形成的一种重要机制[J].地质论评, 2001,47(2):207～209[Liu Chuanlian, Xu Jinli, Wang Pinxian. Algal blooms: the primary mechanism in the formation of lacustrine petroleum source rocks[J].Geological Review, 2001,47(2):207～210]
[25]	Ribouleau A, Derenne S, Largeau C. Origin of contrasting features and preservation pathways in kerogens from the Kashpir oil shales(Upper Jurassic, Russian Platform) [J]. Organic Geochemistry, 2001, 32(5):647～665
[26]	Dahl J E P, Moldowman J M, Teerman S C. Source rock quality determination from oil biomarkers I: a new geochemical technique[J]. AAPG Bulletin, 1994,78(10):1 507～1 526
[27]	Harrison S P,Digerfeldt G. European lake as palaeohydrological and palaeoclimatic indicators[J]. Quaternary Science Review, 1993,12:233～248
[28]	Peters K E, Moldowan J M. The biomarker guide-Interpreting molecular fossils in petroleum and ancient sediments[M]. Prentice Hall, New Jersey. 1993,88
[29]	张立平,黄第藩,廖志勤.伽马蜡烷-水体分层的地球化学标志[J].沉积学报,1999,17(1):136～140[Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerance - geochemical indicator of water column stratification[J]. Acta Sedimentologica Sinica, 1999,17(1):136～140]
[30]	王铁冠.论分子有机地球化学若干名词与术语的辨析和厘定[J].地质论评, 2002,48(3):284～289[Wang Tieguan. Discrimination and stipulation of some terms of molecular organic geochemistry[J]. Geological Review, 2002, 48(3):284～289]
[31]	王慧中,梅洪明.东营凹陷沙三下亚段油页岩中古湖泊学信息[J].同济大学学报,1998,26(3):315～319[Wang Huizhong, Mei Hongming. Paleolimnological information from the oil shale in the lower part of Sha 3 Formation, in Dongying depression[J]. Journal of Tongji University, 1998, 26(3):315～319]

Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression

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