Diagenetic Evolution and Its Influence on Physical Properties of Es4s Reservoir in the Northern Steep Zone of the Bonan Sag

MA BenBen; CAO YingChang; WANG YanZhong; JIA YanCong; ZHANG ShaoMin

doi:10.14027/j.cnki.cjxb.2015.01.018

Volume 33 Issue 1

Turn off MathJax

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2015 > 33(1): 170-182

MA BenBen, CAO YingChang, WANG YanZhong, JIA YanCong, ZHANG ShaoMin. Diagenetic Evolution and Its Influence on Physical Properties of Es4s Reservoir in the Northern Steep Zone of the Bonan Sag[J]. Acta Sedimentologica Sinica, 2015, 33(1): 170-182. doi: 10.14027/j.cnki.cjxb.2015.01.018

Citation:

MA BenBen, CAO YingChang, WANG YanZhong, JIA YanCong, ZHANG ShaoMin. Diagenetic Evolution and Its Influence on Physical Properties of Es₄^s Reservoir in the Northern Steep Zone of the Bonan Sag[J]. Acta Sedimentologica Sinica, 2015, 33(1): 170-182. doi: 10.14027/j.cnki.cjxb.2015.01.018

Diagenetic Evolution and Its Influence on Physical Properties of Es₄^s Reservoir in the Northern Steep Zone of the Bonan Sag

doi: 10.14027/j.cnki.cjxb.2015.01.018

School of Geosciences, China University of Petroleum, Qingdao 266580

Received Date: 2013-08-05
Rev Recd Date: 2014-06-04
Publish Date: 2015-02-10

Abstract

Through the analysis of core observations, thin sections, measured physical properties and combined with the homogenization temperature analysis of fluid-inclusion and burial history in the nearshore subaqueous fan of the Es4s in the northern steep zone of the Bonan sag, the evolution characteristics of diagenesis and reservoir properties was studied. The results showed that, the reservoir diagenesis mainly included strong compaction, lime-mud matrix recrystallization, multi-phase of dissolution and cementation, and complicated metasomatism. The reservoirs have experienced multi-phase acidic and alkaline fluid evolution based on the characteristics of diagenetic environment. In the same diagenetic environment, the difference of sedimentary characteristics in different sub/micro-facies of nearshore subaqueous fan controls the difference of diagenetic evolution characteristics, which also determines the difference of the evolution of reservoir physical property. Based on a method of porosity's inversion and back stripping, physical properties of the reservoirs in geological history were restored, it is shown that compaction, carbonate cementation, lime-mud matrix recrystallization, acid dissolution and former hydrocarbon filling exert the most important effect on the evolution of physical properties. The evolution mode of reservoir physical properties in different sub/micro-facies of nearshore subaqueous fan have been established. The conglomerate in inner fan mainly experiences compaction and lime-mud matrix recrystallization, with weak dissolution, so the physical properties of the conglomerate in inner fan keep reducing and the lime-mud matrix recrystallization results in a rapid reduction of physical properties of the conglomerate in inner fan in middle-deep layers. The present physical property of inner fan becomes extremely poor and mainly develops dry layers. Because two stages of acid dissolution reconstruct the reservoirs and the hydrocarbon filling inhibits cementation, the reservoirs far away from mudstone layers in the braided channels of the middle fan develop a great number of primary and secondary pores, have a higher porosity and permeability, and can be effective reservoirs of hydrocarbon. The reservoirs adjacent to mudstone layers in braided channels of the middle fan, the reservoirs in interdistributaries of the middle fan and outer fan develop intensive cementation and metasomatism, therefore they have poor physical property and mainly develop dry layers.
- diagenesis evolution,
- the evolution of physical property,
- nearshore subaqueous fan,
- Es₄^s,
- Bonan sag

References

[1]	昝灵,张枝焕,王顺华,等. 渤南洼陷北部陡坡带砂砾岩储层成岩作用研究[J]. 天然气地球科学,2011,22(2):299-306. [Zan Ling, Zhang Zhihuan, Wang Shunhua, et al. Diagenesis of sandy conglomerate reservoir in northern steep slope of Bonan subsag[J]. Natural Gas Geoscience, 2011, 22(2): 299-306.]
[2]	仲维苹,操应长,王艳忠,等. 渤南洼陷沙四段沉积砂体类型及分布[J]. 油气地质与采收率,2010,17(1):48-50. [Zhong Weiping, Cao Yingchang, Wang Yanzhong, et al. The types and distribution of the sandbodies in Sha4 member in Bonan depression[J]. Petroleum Geology and Recovery Efficiency, 2010, 17(1): 48-50.]
[3]	郭玉新,隋风贵,林会喜,等. 时频分析技术划分砂砾岩沉积期次方法探讨——以渤南洼陷北部陡坡带沙四段-沙三段为例[J]. 油气地质与采收率,2009,16(5):8-12. [Guo Yuxin, Sui Fenggui, Lin Huixi, et al. Discussion on the division and correlation of glutenite sedimentary period by time-frequency analysis—A case study of Sha4 to Sha3 member of northern abrupt slope zone in Bonan depression[J]. Petroleum Geology and Recovery Efficiency, 2009, 16(5): 8-12.]
[4]	郭瑞超,李延钧,王廷栋,等. 胜利油田渤南洼陷古近系油气源与成藏特征[J]. 新疆石油地质,2009,30(6):674-676. [Guo Ruichao, Li Yanjun, Wang Tingdong, et al. Oil-Gas source and accumulation characteristics of paleogene in Bonan sub-sag in Shengli oil field[J]. Xinjiang Petroleum Geology, 2009, 30(6): 674-676.]
[5]	张枝焕,曾艳涛,张学军,等. 渤海湾盆地沾化凹陷渤南洼陷原油地球化学特征及成藏期分析[J]. 石油实验地质,2006,28(1):54-58. [Zhang Zhihuan, Zeng Yantao, Zhang Xuejun, et al. The geochemistry characteristics and accumulation-history of crude oil in the Bonan sub-sag of the Zhanhua sag, the Bohaiwan Basin[J]. Petroleum Geology & Experiment, 2006, 28(1): 54-58.]
[6]	吴富强,李后蜀,胡雪,等. 沾化凹陷渤南洼陷沙四段成岩史恢复及成岩模式建立[J]. 油气地质与采收率,2001,8(6):1-4. [Wu Fuqiang, Li Houshu, Hu Xue, et al. Diagenetic history of Es₄ in Bonan subsag of Zhanhua sag and establishment of diagenetic model[J]. Petroleum Geology and Recovery Efficiency, 2001, 8(6): 1-4.]
[7]	安爱琴,纪友亮,单敬福. 渤南洼陷沙四上亚段储层成岩作用及物性特征[J]. 上海地质,2007(1):11-16,53. [An Aiqin, Ji Youliang, Shan Jingfu. Diagenesis and physical property characteristics of the upper Sha4 member reservoir in Bonan subsag[J]. Shanghai Geology, 2007(1):11-16, 53.]
[8]	吴富强,汪东波. 胜利油区渤南洼陷沙四上亚段成岩演化序列研究[J]. 华南地质与矿产,2005(1):54-59. [Wu Fuqiang, Wang Dongbo. Diagenetic sequence of the upper Sha4 member in Bonan subsag, Shengli oil field[J]. Geology and Mineral Resources of South China, 2005(1): 54-59.]
[9]	隋风贵,操应长,刘惠民,等. 东营凹陷北带东部古近系近岸水下扇储集物性演化及其油气成藏模式[J]. 地质学报,2010,84(2):246-256. [Sui Fenggui, Cao Yingchang, Liu Huimin, et al. Physical properties evolution and hydrocarbon accumulation of Paleogene nearshore subaqueous fan in the eastern north margin of the Dongying depression[J]. Acta Geologica Sinica, 2010, 84(2): 246-256.]
[10]	Hendry J P, Pearson M J, Trewin N H,et al. Jurassic septarian concretions from NW Scotland record interdependent bacterial, physical and chemical processes of marine mudrock diagenesis[J]. Sedimentology, 2006, 53(3): 537-565.
[11]	孙海涛,钟大康,刘洛夫,等. 沾化凹陷沙河街组砂岩透镜体表面与内部碳酸盐胶结作用的差异及其成因[J]. 石油学报,2010,31(2):246-252. [Sun Haitao, Zhong Dakang, Liu Luofu, et al. Carbonate cementation difference and its origin between exterior and interior surfaces of lenticular sandbody in Shahejie Formation of Zhanhua depression[J]. Acta Petrolei Sinica, 2010, 31(2): 246-252.]
[12]	钟大康,朱筱敏,张琴. 不同埋深条件下砂泥岩互层中砂岩储层物性变化规律[J]. 地质学报,2004,78(6):863-871. [Zhong Dakang, Zhu Xiaomin, Zhang Qin. Variation characteristics of sandstone reservoirs when sandstone and mudstone are interbedded at different buried depths[J]. Acta Geologica Sinica, 2004, 78(6): 863-871.]
[13]	漆滨汶,林春明,邱桂强,等. 东营凹陷古近系沙河街组砂岩透镜体钙质结壳形成机理及其对油气成藏的影响[J]. 古地理学报,2006,8(4):519-529. [Qi Binwen, Lin Chunming, Qiu Guiqiang, et al. Formation mechanism of calcareous incrustation in lenticular sandbody of the Shahejie Formation of Paleogene and its influence on hydrocarbon accumulation in Dongying sag[J]. Journal of Palaeogeography, 2006, 8(4): 519-529.]
[14]	张永旺,曾溅辉,高霞,等. 东营凹陷古近系储层碳酸盐胶结物分布特征及主控因素[J]. 吉林大学学报:地球科学版,2009,39(1):16-22. [Zhang Yongwang, Zeng Jianhui, Gao Xia, et al. Distribution characteristics and main controlling factors of carbonate cements in the Paleogene reservoirs in Dongying Depression[J]. Journal of Jilin University: Earth Science Edition, 2009, 39(1):16-22.]
[15]	Lynch F L, Land L S. Diagenesis of calcite cement in Frio Formation sandstones and its relationship to formation water chemistry[J]. Journal of Sedimentary Research, 1996, 66(3): 439-446.
[16]	姜在兴. 沉积学[M]. 北京:石油工业出版社,2003. [Jiang Zaixing. Sedimentology [M]. Beijing: Petroleum Industry Press, 2003.]
[17]	操应长,贾艳聪,王艳忠,等. 渤南洼陷北带沙四上亚段储层成岩流体演化[J]. 现代地质,2014,28(1):199-200. [Cao Yingchang, Jia Yancong, Wang Yanzhong, et al. Diagenetic fluid evolution of reservoirs in Es₄^s in the north zone of the Bonan sag[J]. Geoscience, 2014, 28(1): 199-200.]
[18]	Hartig K A.Dolomite in Permian paleosols of the Bravo dome CO₂ field, U.S.A.: Permian reflux followed by late recrystallization at elevated temperature[J]. Journal of Sedimentary Research, 2011, 81(4): 248-265.
[19]	邓长瑜,张秀莲,陈建文,等. 黔东南地区寒武系碳酸盐岩成岩作用分析[J]. 沉积学报,2004,22(4):588-596. [Deng Changyu, Zhang Xiulian, Chen Jianwen, et al. The analysis of sequence stratigraphy and diagenesis for the carbonates of Cambrian in the southeast of Guizhou province[J]. Acta Sedimentologica Sinica, 2004, 22(4): 588-596.]
[20]	Fu Qilong. Early dolomitization and recrystallization of carbonate in an evaporite basin: the Middle Devonian Ratner laminite in southern Saskatchewan, Canada[J]. Journal of the Geological Society, London, 2006, 163(6): 937-948.
[21]	郭成贤,王正允,王方平. 深水碳酸盐岩成岩作用的稳定同位素特征[J]. 石油与天然气地质,1999,20(2):144-147. [Guo Chengxian, Wang Zhengyun, Wang Fangping. Stable isotopic characteristics of diagenesis in deep-water carbonate rocks[J]. Oil & Gas Geology, 1999, 20(2): 144-147.]
[22]	李秀华,夏文杰. 砂岩中的杂基类型与鉴别标志[J]. 矿物岩石,1986,6(3):32-40. [Li Xiuhua, Xia Wenjie. The types of matrix in sandstones and their recognitional criteria[J]. Minerals and Rocks, 1986, 6(3): 32-40.]
[23]	Heydari E, Wade W J. Massive recrystallization of low-Mg calcite at high temperatures in hydrocarbon source rocks: Implications for organic acids as factors in diagenesis[J]. AAPG Bulletin, 2002, 86(7): 1285-1303.
[24]	康玉柱. 塔里木盆地古生代海相碳酸盐岩储集岩特征[J]. 石油实验地质,2007,29(3):217-223. [Kang Yuzhu. Reservoir rock characteristics of Paleozoic marine facies carbonate rock in the Tarim Basin[J]. Petroleum Geology & Experiment, 2007, 29(3): 217-223.]
[25]	朱东亚,金之钧,胡文瑄,等. 塔里木盆地深部流体对碳酸盐岩储层影响[J]. 地质论评,2008,54(3):348-357. [Zhu Dongya, Jin Zhijun, Hu Wenxuan, et al. Effects of deep fluid on carbonates reservoir in Tarim Basin[J]. Geological Review, 2008, 54(3): 348-357.]
[26]	刘树根,马永生,王国芝,等. 四川盆地震旦系—下古生界优质储层形成与保存机理[J]. 油气地质与采收率,2008,15(1):1-5. [Liu Shugen, Ma Yongsheng, Wang Guozhi, et al. Formation and conservation mechanism of the high-quality reservoirs in Sinian-Lower Palaeozoic in Sichuan Basin[J]. Petroleum Geology and Recovery Efficiency, 2008, 15(1): 1-5.]
[27]	Raiswell R, Bottrell S H, Dean S P,et al. Isotopic constraints on growth conditions of multiphase calcite-pyrite-barite concretions in Carboniferous mudstones[J]. Sedimentology, 2002, 49(2): 237-254.
[28]	操应长,马奔奔,王艳忠,等. 渤南洼陷北带沙四上亚段储层低渗成因机制及分类评价[J]. 天然气地球科学,2013,24(5):865-875. [Cao Yingchang, Ma Benben, Wang Yanzhong, et al. Genetic mechanisms and classified evaluation of low permeability reservoirs of Es_4s in the north zone of Bonan sag[J]. Natural Gas Geoscience, 2013, 24(5): 865-875.]
[29]	蔡进功,张枝焕,朱筱敏,等. 东营凹陷烃类充注与储集层化学成岩作用[J]. 石油勘探与开发,2003,30(3):79-83. [Cai Jingong, Zhang Zhihuan, Zhu Xiaomin, et al. Hydrocarbon filling and chemical diagenesis evolution of the clastic reservoir of the Paleogene in Dongying sag[J]. Petroleum Exploration and Development, 2003, 30(3): 79-83.]
[30]	张枝焕,胡文瑄,曾溅辉,等. 东营凹陷下第三系流体—岩石相互作用研究[J]. 沉积学报,2000,18(4):560-565. [Zhang Zhihuan, Hu Wenxuan, Zeng Jianhui, et al. Study of fluid-rock interactions in Eogene formation in Dongying depression, Bohai Gulf Basin[J]. Acta Sedimentologica Sinica, 2000, 18(4): 560-565.]
[31]	李艳霞,刘洪军,袁东山,等. 石油充注对储层成岩矿物演化的影响[J]. 石油与天然气地质,2003,24(3):274-280. [Li Yanxia, Liu Hongjun, Yuan Dongshan, et al. Effect of oil charging on reservoir's diagenetic mineral evolution[J]. Oil & Gas Geology, 2003, 24(4): 274-280.]
[32]	吴富强,宁兴贤. 影响渤南洼陷深部储层次生孔隙形成的因素及其作用[J]. 沉积与特提斯地质,2004,24(2):76-82. [Wu Fuqiang, Ning Xingxian. The controlling factors and processes for the formation of the secondary porosity of the deep-seated reservoir rocks in the Bonan depression, Shandong[J]. Sedimentary Geology and Tethyan Geology, 2001, 24(2): 76-82.]
[33]	王艳忠,操应长,葸克来,等. 碎屑岩储层地质历史时期孔隙度演化恢复方法——以济阳坳陷东营凹陷沙河街组四段上亚段为例[J]. 石油学报,2013,34(6):1100-1110. [Wang Yanzhong, Cao Yingchang, Xi Kelai, et al. A recovery method for porosity evolution of clastic reservoirs with geological time: A case study from the upper part submember of Es4 in the Dongying depression, Jiyang subbasin[J]. Acta Petrolei Sinica, 2013, 34(6): 1100-1110.]

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article Metrics

Article views(1038) PDF downloads(833) Cited by()

Proportional views

Diagenetic Evolution and Its Influence on Physical Properties of Es₄^s Reservoir in the Northern Steep Zone of the Bonan Sag

School of Geosciences, China University of Petroleum, Qingdao 266580

Received Date: 2013-08-05

Rev Recd Date: 2014-06-04

Publish Date: 2015-02-10

Key words:

Abstract: Through the analysis of core observations, thin sections, measured physical properties and combined with the homogenization temperature analysis of fluid-inclusion and burial history in the nearshore subaqueous fan of the Es4s in the northern steep zone of the Bonan sag, the evolution characteristics of diagenesis and reservoir properties was studied. The results showed that, the reservoir diagenesis mainly included strong compaction, lime-mud matrix recrystallization, multi-phase of dissolution and cementation, and complicated metasomatism. The reservoirs have experienced multi-phase acidic and alkaline fluid evolution based on the characteristics of diagenetic environment. In the same diagenetic environment, the difference of sedimentary characteristics in different sub/micro-facies of nearshore subaqueous fan controls the difference of diagenetic evolution characteristics, which also determines the difference of the evolution of reservoir physical property. Based on a method of porosity's inversion and back stripping, physical properties of the reservoirs in geological history were restored, it is shown that compaction, carbonate cementation, lime-mud matrix recrystallization, acid dissolution and former hydrocarbon filling exert the most important effect on the evolution of physical properties. The evolution mode of reservoir physical properties in different sub/micro-facies of nearshore subaqueous fan have been established. The conglomerate in inner fan mainly experiences compaction and lime-mud matrix recrystallization, with weak dissolution, so the physical properties of the conglomerate in inner fan keep reducing and the lime-mud matrix recrystallization results in a rapid reduction of physical properties of the conglomerate in inner fan in middle-deep layers. The present physical property of inner fan becomes extremely poor and mainly develops dry layers. Because two stages of acid dissolution reconstruct the reservoirs and the hydrocarbon filling inhibits cementation, the reservoirs far away from mudstone layers in the braided channels of the middle fan develop a great number of primary and secondary pores, have a higher porosity and permeability, and can be effective reservoirs of hydrocarbon. The reservoirs adjacent to mudstone layers in braided channels of the middle fan, the reservoirs in interdistributaries of the middle fan and outer fan develop intensive cementation and metasomatism, therefore they have poor physical property and mainly develop dry layers.

HTML

Reference (33)

[1]	昝灵,张枝焕,王顺华,等. 渤南洼陷北部陡坡带砂砾岩储层成岩作用研究[J]. 天然气地球科学,2011,22(2):299-306. [Zan Ling, Zhang Zhihuan, Wang Shunhua, et al. Diagenesis of sandy conglomerate reservoir in northern steep slope of Bonan subsag[J]. Natural Gas Geoscience, 2011, 22(2): 299-306.]
[2]	仲维苹,操应长,王艳忠,等. 渤南洼陷沙四段沉积砂体类型及分布[J]. 油气地质与采收率,2010,17(1):48-50. [Zhong Weiping, Cao Yingchang, Wang Yanzhong, et al. The types and distribution of the sandbodies in Sha4 member in Bonan depression[J]. Petroleum Geology and Recovery Efficiency, 2010, 17(1): 48-50.]
[3]	郭玉新,隋风贵,林会喜,等. 时频分析技术划分砂砾岩沉积期次方法探讨——以渤南洼陷北部陡坡带沙四段-沙三段为例[J]. 油气地质与采收率,2009,16(5):8-12. [Guo Yuxin, Sui Fenggui, Lin Huixi, et al. Discussion on the division and correlation of glutenite sedimentary period by time-frequency analysis—A case study of Sha4 to Sha3 member of northern abrupt slope zone in Bonan depression[J]. Petroleum Geology and Recovery Efficiency, 2009, 16(5): 8-12.]
[4]	郭瑞超,李延钧,王廷栋,等. 胜利油田渤南洼陷古近系油气源与成藏特征[J]. 新疆石油地质,2009,30(6):674-676. [Guo Ruichao, Li Yanjun, Wang Tingdong, et al. Oil-Gas source and accumulation characteristics of paleogene in Bonan sub-sag in Shengli oil field[J]. Xinjiang Petroleum Geology, 2009, 30(6): 674-676.]
[5]	张枝焕,曾艳涛,张学军,等. 渤海湾盆地沾化凹陷渤南洼陷原油地球化学特征及成藏期分析[J]. 石油实验地质,2006,28(1):54-58. [Zhang Zhihuan, Zeng Yantao, Zhang Xuejun, et al. The geochemistry characteristics and accumulation-history of crude oil in the Bonan sub-sag of the Zhanhua sag, the Bohaiwan Basin[J]. Petroleum Geology & Experiment, 2006, 28(1): 54-58.]
[6]	吴富强,李后蜀,胡雪,等. 沾化凹陷渤南洼陷沙四段成岩史恢复及成岩模式建立[J]. 油气地质与采收率,2001,8(6):1-4. [Wu Fuqiang, Li Houshu, Hu Xue, et al. Diagenetic history of Es₄ in Bonan subsag of Zhanhua sag and establishment of diagenetic model[J]. Petroleum Geology and Recovery Efficiency, 2001, 8(6): 1-4.]
[7]	安爱琴,纪友亮,单敬福. 渤南洼陷沙四上亚段储层成岩作用及物性特征[J]. 上海地质,2007(1):11-16,53. [An Aiqin, Ji Youliang, Shan Jingfu. Diagenesis and physical property characteristics of the upper Sha4 member reservoir in Bonan subsag[J]. Shanghai Geology, 2007(1):11-16, 53.]
[8]	吴富强,汪东波. 胜利油区渤南洼陷沙四上亚段成岩演化序列研究[J]. 华南地质与矿产,2005(1):54-59. [Wu Fuqiang, Wang Dongbo. Diagenetic sequence of the upper Sha4 member in Bonan subsag, Shengli oil field[J]. Geology and Mineral Resources of South China, 2005(1): 54-59.]
[9]	隋风贵,操应长,刘惠民,等. 东营凹陷北带东部古近系近岸水下扇储集物性演化及其油气成藏模式[J]. 地质学报,2010,84(2):246-256. [Sui Fenggui, Cao Yingchang, Liu Huimin, et al. Physical properties evolution and hydrocarbon accumulation of Paleogene nearshore subaqueous fan in the eastern north margin of the Dongying depression[J]. Acta Geologica Sinica, 2010, 84(2): 246-256.]
[10]	Hendry J P, Pearson M J, Trewin N H,et al. Jurassic septarian concretions from NW Scotland record interdependent bacterial, physical and chemical processes of marine mudrock diagenesis[J]. Sedimentology, 2006, 53(3): 537-565.
[11]	孙海涛,钟大康,刘洛夫,等. 沾化凹陷沙河街组砂岩透镜体表面与内部碳酸盐胶结作用的差异及其成因[J]. 石油学报,2010,31(2):246-252. [Sun Haitao, Zhong Dakang, Liu Luofu, et al. Carbonate cementation difference and its origin between exterior and interior surfaces of lenticular sandbody in Shahejie Formation of Zhanhua depression[J]. Acta Petrolei Sinica, 2010, 31(2): 246-252.]
[12]	钟大康,朱筱敏,张琴. 不同埋深条件下砂泥岩互层中砂岩储层物性变化规律[J]. 地质学报,2004,78(6):863-871. [Zhong Dakang, Zhu Xiaomin, Zhang Qin. Variation characteristics of sandstone reservoirs when sandstone and mudstone are interbedded at different buried depths[J]. Acta Geologica Sinica, 2004, 78(6): 863-871.]
[13]	漆滨汶,林春明,邱桂强,等. 东营凹陷古近系沙河街组砂岩透镜体钙质结壳形成机理及其对油气成藏的影响[J]. 古地理学报,2006,8(4):519-529. [Qi Binwen, Lin Chunming, Qiu Guiqiang, et al. Formation mechanism of calcareous incrustation in lenticular sandbody of the Shahejie Formation of Paleogene and its influence on hydrocarbon accumulation in Dongying sag[J]. Journal of Palaeogeography, 2006, 8(4): 519-529.]
[14]	张永旺,曾溅辉,高霞,等. 东营凹陷古近系储层碳酸盐胶结物分布特征及主控因素[J]. 吉林大学学报:地球科学版,2009,39(1):16-22. [Zhang Yongwang, Zeng Jianhui, Gao Xia, et al. Distribution characteristics and main controlling factors of carbonate cements in the Paleogene reservoirs in Dongying Depression[J]. Journal of Jilin University: Earth Science Edition, 2009, 39(1):16-22.]
[15]	Lynch F L, Land L S. Diagenesis of calcite cement in Frio Formation sandstones and its relationship to formation water chemistry[J]. Journal of Sedimentary Research, 1996, 66(3): 439-446.
[16]	姜在兴. 沉积学[M]. 北京:石油工业出版社,2003. [Jiang Zaixing. Sedimentology [M]. Beijing: Petroleum Industry Press, 2003.]
[17]	操应长,贾艳聪,王艳忠,等. 渤南洼陷北带沙四上亚段储层成岩流体演化[J]. 现代地质,2014,28(1):199-200. [Cao Yingchang, Jia Yancong, Wang Yanzhong, et al. Diagenetic fluid evolution of reservoirs in Es₄^s in the north zone of the Bonan sag[J]. Geoscience, 2014, 28(1): 199-200.]
[18]	Hartig K A.Dolomite in Permian paleosols of the Bravo dome CO₂ field, U.S.A.: Permian reflux followed by late recrystallization at elevated temperature[J]. Journal of Sedimentary Research, 2011, 81(4): 248-265.
[19]	邓长瑜,张秀莲,陈建文,等. 黔东南地区寒武系碳酸盐岩成岩作用分析[J]. 沉积学报,2004,22(4):588-596. [Deng Changyu, Zhang Xiulian, Chen Jianwen, et al. The analysis of sequence stratigraphy and diagenesis for the carbonates of Cambrian in the southeast of Guizhou province[J]. Acta Sedimentologica Sinica, 2004, 22(4): 588-596.]
[20]	Fu Qilong. Early dolomitization and recrystallization of carbonate in an evaporite basin: the Middle Devonian Ratner laminite in southern Saskatchewan, Canada[J]. Journal of the Geological Society, London, 2006, 163(6): 937-948.
[21]	郭成贤,王正允,王方平. 深水碳酸盐岩成岩作用的稳定同位素特征[J]. 石油与天然气地质,1999,20(2):144-147. [Guo Chengxian, Wang Zhengyun, Wang Fangping. Stable isotopic characteristics of diagenesis in deep-water carbonate rocks[J]. Oil & Gas Geology, 1999, 20(2): 144-147.]
[22]	李秀华,夏文杰. 砂岩中的杂基类型与鉴别标志[J]. 矿物岩石,1986,6(3):32-40. [Li Xiuhua, Xia Wenjie. The types of matrix in sandstones and their recognitional criteria[J]. Minerals and Rocks, 1986, 6(3): 32-40.]
[23]	Heydari E, Wade W J. Massive recrystallization of low-Mg calcite at high temperatures in hydrocarbon source rocks: Implications for organic acids as factors in diagenesis[J]. AAPG Bulletin, 2002, 86(7): 1285-1303.
[24]	康玉柱. 塔里木盆地古生代海相碳酸盐岩储集岩特征[J]. 石油实验地质,2007,29(3):217-223. [Kang Yuzhu. Reservoir rock characteristics of Paleozoic marine facies carbonate rock in the Tarim Basin[J]. Petroleum Geology & Experiment, 2007, 29(3): 217-223.]
[25]	朱东亚,金之钧,胡文瑄,等. 塔里木盆地深部流体对碳酸盐岩储层影响[J]. 地质论评,2008,54(3):348-357. [Zhu Dongya, Jin Zhijun, Hu Wenxuan, et al. Effects of deep fluid on carbonates reservoir in Tarim Basin[J]. Geological Review, 2008, 54(3): 348-357.]
[26]	刘树根,马永生,王国芝,等. 四川盆地震旦系—下古生界优质储层形成与保存机理[J]. 油气地质与采收率,2008,15(1):1-5. [Liu Shugen, Ma Yongsheng, Wang Guozhi, et al. Formation and conservation mechanism of the high-quality reservoirs in Sinian-Lower Palaeozoic in Sichuan Basin[J]. Petroleum Geology and Recovery Efficiency, 2008, 15(1): 1-5.]
[27]	Raiswell R, Bottrell S H, Dean S P,et al. Isotopic constraints on growth conditions of multiphase calcite-pyrite-barite concretions in Carboniferous mudstones[J]. Sedimentology, 2002, 49(2): 237-254.
[28]	操应长,马奔奔,王艳忠,等. 渤南洼陷北带沙四上亚段储层低渗成因机制及分类评价[J]. 天然气地球科学,2013,24(5):865-875. [Cao Yingchang, Ma Benben, Wang Yanzhong, et al. Genetic mechanisms and classified evaluation of low permeability reservoirs of Es_4s in the north zone of Bonan sag[J]. Natural Gas Geoscience, 2013, 24(5): 865-875.]
[29]	蔡进功,张枝焕,朱筱敏,等. 东营凹陷烃类充注与储集层化学成岩作用[J]. 石油勘探与开发,2003,30(3):79-83. [Cai Jingong, Zhang Zhihuan, Zhu Xiaomin, et al. Hydrocarbon filling and chemical diagenesis evolution of the clastic reservoir of the Paleogene in Dongying sag[J]. Petroleum Exploration and Development, 2003, 30(3): 79-83.]
[30]	张枝焕,胡文瑄,曾溅辉,等. 东营凹陷下第三系流体—岩石相互作用研究[J]. 沉积学报,2000,18(4):560-565. [Zhang Zhihuan, Hu Wenxuan, Zeng Jianhui, et al. Study of fluid-rock interactions in Eogene formation in Dongying depression, Bohai Gulf Basin[J]. Acta Sedimentologica Sinica, 2000, 18(4): 560-565.]
[31]	李艳霞,刘洪军,袁东山,等. 石油充注对储层成岩矿物演化的影响[J]. 石油与天然气地质,2003,24(3):274-280. [Li Yanxia, Liu Hongjun, Yuan Dongshan, et al. Effect of oil charging on reservoir's diagenetic mineral evolution[J]. Oil & Gas Geology, 2003, 24(4): 274-280.]
[32]	吴富强,宁兴贤. 影响渤南洼陷深部储层次生孔隙形成的因素及其作用[J]. 沉积与特提斯地质,2004,24(2):76-82. [Wu Fuqiang, Ning Xingxian. The controlling factors and processes for the formation of the secondary porosity of the deep-seated reservoir rocks in the Bonan depression, Shandong[J]. Sedimentary Geology and Tethyan Geology, 2001, 24(2): 76-82.]
[33]	王艳忠,操应长,葸克来,等. 碎屑岩储层地质历史时期孔隙度演化恢复方法——以济阳坳陷东营凹陷沙河街组四段上亚段为例[J]. 石油学报,2013,34(6):1100-1110. [Wang Yanzhong, Cao Yingchang, Xi Kelai, et al. A recovery method for porosity evolution of clastic reservoirs with geological time: A case study from the upper part submember of Es4 in the Dongying depression, Jiyang subbasin[J]. Acta Petrolei Sinica, 2013, 34(6): 1100-1110.]

Diagenetic Evolution and Its Influence on Physical Properties of Es₄^s Reservoir in the Northern Steep Zone of the Bonan Sag

doi: 10.14027/j.cnki.cjxb.2015.01.018

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Diagenetic Evolution and Its Influence on Physical Properties of Es₄^s Reservoir in the Northern Steep Zone of the Bonan Sag

doi: 10.14027/j.cnki.cjxb.2015.01.018

School of Geosciences, China University of Petroleum, Qingdao 266580

HTML

Catalog

Links

Journal Online

Contact Us

Diagenetic Evolution and Its Influence on Physical Properties of Es4s Reservoir in the Northern Steep Zone of the Bonan Sag

doi: 10.14027/j.cnki.cjxb.2015.01.018

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Publishing history