东营凹陷中央隆起带沙河街组碳酸盐胶结物发育特征及其形成机制

郭佳; 曾溅辉; 宋国奇; 张永旺; 王学军; 孟伟

doi:10.3799/dqkx.2014.054

Volume 39 Issue 5

May 2014

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Guo Jia, Zeng Jianhui, Song Guoqi, Zhang Yongwang, Wang Xuejun, Meng Wei, 2014. Characteristics and Origin of Carbonate Cements of Shahejie Formation of Central Uplift Belt in Dongying Depression. Earth Science, 39(5): 565-576. doi: 10.3799/dqkx.2014.054

Citation:

Guo Jia, Zeng Jianhui, Song Guoqi, Zhang Yongwang, Wang Xuejun, Meng Wei, 2014. Characteristics and Origin of Carbonate Cements of Shahejie Formation of Central Uplift Belt in Dongying Depression. Earth Science, 39(5): 565-576. doi: 10.3799/dqkx.2014.054

Citation:

Guo Jia, Zeng Jianhui, Song Guoqi, Zhang Yongwang, Wang Xuejun, Meng Wei, 2014. Characteristics and Origin of Carbonate Cements of Shahejie Formation of Central Uplift Belt in Dongying Depression. Earth Science, 39(5): 565-576. doi: 10.3799/dqkx.2014.054

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Characteristics and Origin of Carbonate Cements of Shahejie Formation of Central Uplift Belt in Dongying Depression

doi: 10.3799/dqkx.2014.054

Guo Jia^{1, 2
,},
Zeng Jianhui^{1, 2
,
,},
Song Guoqi³,
Zhang Yongwang^{1, 2},
Wang Xuejun⁴,
Meng Wei^{1, 2}

1.
State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
2.
College of Geosciences, China University of Petroleum, Beijing 102249, China
3.
Shengli Oilfield Branch Company, SINOPEC, Dongying 257000, China
4.
Geological Scientific Research Institute of Shengli Oilfield, SINOPEC, Dongying 257015, China

Received Date: 2013-10-11
Publish Date: 2014-05-01

Abstract

Abstract

Carbonate cement is an important authigenic mineral in sandstone reservoirs of the central uplift belt in the Dongying depression, but no in-depth study has been conducted on its formation mechanisms currently. In this article, carbonate cements of Shahejie Formation of the central uplift belt in the Dongying depression are divided into four periods using petrologic records and their development characteristics are concluded. And then, according to the paragenetic mineral assemblages, carbon and oxygen isotope ratios, chemical elemental composition and other information of carbonate cements, their formation mechanisms were studied. Study results show that carbonates in the study area are mainly affected by the organic acids generated during the process of maturation of organic matter and the dissolution of the carbonate debris during deposition of Es₄. In the study area, four periods of carbonate cements developed mostly. The first period of carbonate cements is mainly dolomite. Its formation is related to decomposition effects of methane bacteria on organic matter; the second period of carbonate cements is mainly formed of calcite and there is a layer of chlorite film locating between the second period and the first period of carbonate cements. The formation of cements is related to Ca and HCO₃^- oversaturation caused by pore fluid condensation; the third period of carbonate cements mainly include calcite, dolomite and ankerite, being characterized by filling dissolution pore of feldspar and primary pore, with their substance derived from the dissolution pore of feldspar and dehydration of mudstone; the fourth period of carbonate cements is characterized by filling the early-stage carbonate-corroded pores. Their substances are derived from the conversion of clay minerals and are usually symbiotic with pyrite particles, and their formation is affected by the hydrocarbon fluid flow.
- carbonate,
- cement,
- distribution characteristic,
- formation mechanism,
- Shahejie Formation,
- central uplift belt of Dongying depression

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References(48)

References

Anna, B., Susanne, G., Peter, K., 2009. Porosity-Preserving Chlorite Cements in Shallow-Marine Volcaniclastic Sandstones: Evidence from Cretaceous Sandstones of the Sawan Gas Field, Pakistan. AAPG Bulletin, 93(5): 595-615. doi: 10.1306/01300908096

Cai, G.Q., Guo, F., Liu, X.T., et al., 2009. Carbon and Oxygen Isotope Characteristics and Palaeoenvironmental Implications of Lacustrine Carbonate Rocks from the Shahejie Formation in the Dongying Sag. Earth and Environment, 37(4): 347-354(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZDQ200904006.htm

Chen, Y.Q., Yu, X.H., Zhou, X.G., et al., 2004. Research on Diagenetic Evolutive Succession and Occurrence of Secondary Porosity of Lower Tertiary in Different Structural Belt of Dongying Depression. Natural Gas Geoscience, 15(1): 68-74(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TDKX200401013.htm

Denies, P., 1980. The Isotopic Composition of Reduced Organic Carbon. In: Fritz, P., Fontes, J.C., eds., Handbook of Environmental Isotope Geochemistry, Vol. 1, The Terrestrial Environment. Elsevier Scientific Publishing Company, Amsterdam, 339-345.

Drummod, C.N., Wilkinson, B.H., Lohmann, K.C., et al., 1993. Effect of Regional Topography and Hydrology on the Lacustrine Isotopic Record of Miocene Paleoclimate in Rocky Mountains. Palaeogeogr., Palaeoclimatol., Palaeoecal. , 101(1-2): 67-79. doi: 10.1016/0031-0182(93)90152-9

Fayek, M., Harrison, T.M., Grove, M., et al., 2001. In Situ Stable Isotopic Evidence for Protracted and Complex Carbonate Cementation in a Protracted and Complex Carbonate Cementation in a Petroleum Reservoir, North Coles Levee, San Joaquin Basin, California, USA. Journal of Sedimentary Research, 71(3): 444-458. doi: 10.1306/2DC40954-0E47-11D7-8643000102C1865D

Frank, S.G., Dias, R., Freeman, K.H., et al., 2011. Carbon Isotopic Composition of Organic Acids in Oil Field Waters, San Joaquin Basin, California, USA. Geochimica et Cosmochimica Acta, 65(8): 1301-1310. doi: 10.1016/S0016-7037(00)00606-2

Han, Y.J., He, S., Song, G.Q., et al., 2012. Origin of Carbonate Cements in the Overpressured Top Seal and Adjacent Sandstones in Dongying Depression. Acta Petrolei Sinica, 33(3): 385-393(in Chinese with English abstract). doi: 10.1038/aps.2011.162

He, S., Yang, Z., He, Z.L., et al., 2009. Mechanism of Carbonate Cementation and Secondary Dissolution Porosity Formation in Deep-Burial Sandstones near the Top Overpressured Surface in Central Part of Junggar Basin. Earth Science-Journal of China University of Geosciences, 34(5): 759-768, 798(in Chinese with English abstract). doi: 10.3799/dqkx.2009.084

Hoefs, J., 1997. Stable Isotope Geochemistry. Springer-Verlag, Berlin.

Huang, S.J., Qing, H.R., Hu, Z.W., et al., 2008. Cathodoluminescence and Diagenesis of the Carbonate Rocks in Feixianguan Formation of Triassic, Eastern Sichuan Basin of China. Earth Science-Journal of China University of Geosciences, 33(1): 26-34(in Chinese with English abstract). doi: 10.3799/dqkx.2008.004

Kelts, K., Talbot, M., 1990. Lacustrine Carbonates as Geochemical Archives of Environmental Change and Biotic/ Biotic Interactions. In: Tilzer, M.M., Serruya, C., eds., Large Lakes: Ecological Structure and Function. Springer-Verlag, New York, 288-315. doi: 10.1007/978-3-642-84077-7_15

Li, P.L., Jiang, Z.X., Ma, Z.P., et al., 2000. Reservoir and Oil & Gas Distribution in Dongying Sag. Petroleum Industry Press, Beijing, 11-35(in Chinese).

Li, Z.Q., Chen, H.H., Liu, H.M., et al., 2008. Division of Hydrocarbon Charges and Charging Date Determination of Sha 3 Member, Dongying Depression by Various Aspects of Fluid Inclusions. Geological Science and Technology Information, 27(4): 69-74(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ200804013.htm

Ma, L.J., Zheng, H.R., Xie, X.N., 2005. Faulted Structures and Hydrocarbon Migration in Central Uplift Belt of Dongying Depression. Oil & Gas Geology, 26(2): 246-251 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200502020.htm

Morad, S., 1998. Carbonate Cementation in Sandstones: Distribution Patterns and Geochemical Evolution (Special Publication 26 of the IAS). Wiley-Blackwell Press, New Jersey, 1-26.

Pan, L.Y., Huang, G.P., Shou, J.F., et al., 2009. A Preliminary Study of Formation Environment of the Neogene Lacustrine Carbonates in Nanyishan Area of Qaidam Basin: Constrains from Carbon-Oxygen Isotope and Fluid Inclusion Analysis. Bulletin of Mineralogy, Petrology and Geochemistry, 28(1): 71-74(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KYDH200901014.htm

Taylor, H.P., Frechen, J., Degens, E.T., 1967. Oxygen and Carbon Isotope Studies of Carbonatites from the Laacher See District, West Germany and the Alnö District, Sweden. Geochimica et Cosmochimica Acta, 31(3): 407-430. doi: 10.1016/0016-7037(67)90051-8

Toyoda, K., Horichi, H., Tokonami, M., 1994. Dupal Anomaly of Brazilian Carbonatites Geochemical Correlations with Hotspots in the South Atlantic and Implications for the Mantle Source. Earth and Planetary Science Letter, 126(4): 315-331. doi: 10.1016/0012-821X(94)90115-5

Valley, J.W., 1986. Stable Isotope Geochemistry of Metamorphic Rocks. In: Valley, J.W., Clayton, R.N., O'Neil, J.R., eds., Stable Isotopes in High Temperature Geological Processes. Reviews in Mineralogy and Geochemistry, USA, 16: 445-489.

Veizer, J., Hoefs, J., 1976. The Nature of O¹⁸/O¹⁶ and C¹³/C¹² Secular Trends in Sedimentary Carbonate Rocks. Geochimica et Cosmochimica Acta, 40(11): 1387-1395. doi: 10.1016/0016-7037(76)90129-0

Wang, D.R., Zhang, Y.H., 2001. A Study on the Origin of the Carbonate Cements within Reservoirs in the External Metamorphic Belt of the Bohai Bay Oil-Gas Bearing Region. Petroleum Exploration and Development, 28(2): 40-42(in Chinese with English abstract).

Wang, Q.B., Zang, C.Y., Lai, W.C., et al., 2009. Distribution Characteristics and Origin of Carbonate Cements in the Middle and Deep Clastic Reservoirs of the Paleogene in the Bozhong Depression. Oil & Gas Geology, 30(4): 438-443(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200904012.htm

Yang, X.Z., Yang, Z.L., Tao, K.Y., et al., 2002. Formation Temperature of Chloritein Oil-Bearing Basalt. Acta Mineralogica Sinica, 22(4): 365-370(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWXB200204012.htm

You, G.Q., Pan, J.H., Liu, S.Q., et al., 2006. Diagenesis and Pore Evolution of Paleogene Sandstone Reservoir in Dongying Depression. Acta Petrologica et Mineralogica, 25(3): 237-242(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200603008.htm

Yu, B.S., Lai, X.Y., Gao, Z.Q., 2007. The Equilibrium between Calcite and Dolomite during Diagenesis in Sandstone Reservoir in Kela 2 Gas Field and the Influence to Quality of Reservoir. Progress in Natural Science, 17(3): 339-345(in Chinese). http://en.cnki.com.cn/Article_en/CJFDTotal-ZKJY200709009.htm

Zeng, J.H., Peng, J.L., Qiu, N.S., et al., 2006. Carbonate Dissolution-Precipitation in Sandstone-Shale Contact and Its Petroleum Geological Meanings. Natural Gas Geoscicence, 17(6): 760-764(in Chinese with English abstract). http://www.oalib.com/paper/1418040

Zhang, Y.W., Zeng, J.H., Gao, X., et al., 2009. Distribution Characteristics and Main Controlling Factors of Carbonate Cements in the Paleogene Reservoirs in Dongying Depression. Journal of Jilin University (Earth Science Edition), 39(1): 16-22(in Chinese with English abstract). http://www.cqvip.com/QK/91256B/200901/29246857.html

Zhong, D.K., Zhu, X.M., Zhang, Z.H., et al., 2003. Controlling Factors of Sandstone Reservoir of the Paleogene in Dongying Sag. Petroleum Exploration and Development, 30(3): 95-98(in Chinese with English abstract).

Zhu, H.Q., Pang, X.Q., Jiang, Z.X., et al., 2007. Accumulation Time and Accumulation Process of Lithological Reservoirs in Dongying Depression. Geological Science and Technology Information, 26(1): 65-70(in Chinese with English abstract).

蔡观强, 郭峰, 刘显太, 等, 2009. 东营凹陷沙河街组沉积岩碳氧同位素组成的古环境记录. 地球与环境, 37(4): 347-354. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ200904006.htm

陈永峤, 于兴河, 周新桂, 等, 2004. 东营凹陷各构造区带下第三系成岩演化与次生孔隙发育规律研究. 天然气地球科学, 15(1): 68-74. doi: 10.3969/j.issn.1672-1926.2004.01.013

韩元佳, 何生, 宋国奇, 等, 2012. 东营凹陷超压顶封层及其附近砂岩中碳酸盐胶结物的成因. 石油学报, 33(3): 385-393. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201203006.htm

何生, 杨智, 何志亮, 等, 2009. 准噶尔盆地腹部超压顶面附近深层砂岩碳酸盐胶结作用和次生溶蚀孔隙形成机理. 地球科学—中国地质大学学报, 34(5): 759-768, 798. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200905008.htm

黄思静, 卿海若, 胡作维, 等, 2008. 川东三叠系飞仙关组碳酸盐岩的阴极发光特征与成岩作用. 地球科学—中国地质大学学报, 33(1): 26-34. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200801007.htm

李丕龙, 姜在兴, 马在平, 等, 2000. 东营凹陷储集体与油气分布. 北京: 石油工业出版社, 11-35.

李兆奇, 陈红汉, 刘惠民, 等, 2008. 流体包裹体多参数综合划分东营凹陷沙三段油气充注期次及充注时期确定. 地质科技情报, 27(4): 69-74. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200804013.htm

马丽娟, 郑和荣, 解习农, 2005. 东营凹陷中央隆起带断裂构造及油气运移. 石油与天然气地质, 26(2): 246-251. doi: 10.3321/j.issn:0253-9985.2005.02.021

潘立银, 黄革萍, 寿建峰, 等, 2009. 柴达木盆地南翼山地区新近系湖相碳酸盐岩成岩环境初探—碳、氧同位素和流体包裹体证据. 矿物岩石地球化学通报, 28(1): 71-74. doi: 10.3969/j.issn.1007-2802.2009.01.011

王大锐, 张映红, 2001. 渤海湾油气区火成岩外变质带储集层中碳酸盐胶结物成因研究及意义. 石油勘探与开发, 28(2): 40-42. doi: 10.3321/j.issn:1000-0747.2001.02.012

王清斌, 臧春艳, 赖维成, 等, 2009. 渤中坳陷古近系中、深部碎屑岩储层碳酸盐胶结物分布特征及成因机制. 石油与天然气地质, 30(4): 438-443. doi: 10.3321/j.issn:0253-9985.2009.04.008

杨献忠, 杨祝良, 陶奎元, 等, 2002. 含油玄武岩中绿泥石的形成温度. 矿物学报, 22(4): 365-370. doi: 10.3321/j.issn:1000-4734.2002.04.012

游国庆, 潘家华, 刘淑琴, 等, 2006. 东营凹陷古近系砂岩成岩作用与孔隙演化. 岩石矿物学杂志, 25(3): 237-242. doi: 10.3969/j.issn.1000-6524.2006.03.009

于炳松, 赖兴运, 高志前, 等, 2007. 克拉2气田砂岩储层中成岩方解石-白云石的平衡及其对储层质量的影响. 自然科学进展, 17(3): 339-345. doi: 10.3321/j.issn:1002-008X.2007.03.008

曾溅辉, 彭继林, 邱楠生, 等, 2006. 砂-泥岩界面碳酸盐溶解-沉淀反应及其石油地质意义. 天然气地球科学, 17(6): 760-764. doi: 10.3969/j.issn.1672-1926.2006.06.004

张永旺, 曾溅辉, 高霞, 等, 2009. 东营凹陷古近系储层碳酸盐胶结物分布特征及主控因素. 吉林大学学报(地球科学版), 39(1): 16-22. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200901003.htm

钟大康, 朱筱敏, 张枝焕, 等, 2003. 东营凹陷古近系砂岩储集层物性控制因素评价. 石油勘探与开发, 30(3): 95-98. doi: 10.3321/j.issn:1000-0747.2003.03.026

祝厚勤, 庞雄奇, 姜振学, 等, 2007. 东营凹陷岩性油藏成藏期次与成藏过程. 地质科技情报, 26(1): 65-70. doi: 10.3969/j.issn.1000-7849.2007.01.011

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Characteristics and Origin of Carbonate Cements of Shahejie Formation of Central Uplift Belt in Dongying Depression

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