渤海湾盆地黄河口凹陷沙河街组白云岩成因机理

姚婷婷; 朱红涛; 杨香华; 石文龙; 牛成民

doi:10.3799/dqkx.2020.227

Volume 45 Issue 10

Nov. 2020

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2020 > 45(10): 3567-3578

Yao Tingting, Zhu Hongtao, Yang Xianghua, Shi Wenlong, Niu Chengmin, 2020. Dolomite Origin of Shahejie Formation in Huanghekou Sag, Bohai Bay Basin. Earth Science, 45(10): 3567-3578. doi: 10.3799/dqkx.2020.227

Citation:

Yao Tingting, Zhu Hongtao, Yang Xianghua, Shi Wenlong, Niu Chengmin, 2020. Dolomite Origin of Shahejie Formation in Huanghekou Sag, Bohai Bay Basin. Earth Science, 45(10): 3567-3578. doi: 10.3799/dqkx.2020.227

Citation:

PDF( 20794 KB)

Dolomite Origin of Shahejie Formation in Huanghekou Sag, Bohai Bay Basin

doi: 10.3799/dqkx.2020.227

Yao Tingting^{1, 2
,
,},
Zhu Hongtao^{1, 2
,
,},
Yang Xianghua^{1, 2},
Shi Wenlong³,
Niu Chengmin³

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
Tianjin Branch of China National Offshore Oil Corporation Limited, Tianjin 300459, China

Received Date: 2020-04-20
Publish Date: 2020-11-17

Abstract

Abstract

To study the dolomite origin of Shahejie Formation in Huanghekou sag, Bohai Bay basin, the petrology, morphology and isotopic geochemical characteristics of the dolomite were analyzed through core observation, thin section identification, cathodoluminescence, X-ray diffractometry (XRD), scanning electron microscopy (SEM), back-scattered electrons (BSE) and carbon and oxygen isotopes. The results show that the dolomite is yellow brown and has a lot of dissolution pores, chert and kaolinite develops. δ¹³C values range from -0.50‰ to 4.58‰, and δ¹⁸O values range from -14.58‰ to -2.19‰. Micritic dolomite consists of microsphere dolomite and dolomized cyanbacteria accompanied with a lot of submicron pores, sheet-like bacterial filaments and strawberry pyrite. Fibrous isopachous dolomite cements fill in the dissolution pores or grow around particle surfaces. Rhombic dolomite is dispersed in pores. During penecontemporaneous stage, sulfate reducing bacteria induced spherical dolomite precipitation. Subsequently, fibrous isopachous dolomite cements were influenced by microbes under lake floor diagenetic environment, being affected by meteoric fresh water. During shallow burial stage, rhombic dolomite precipitates by buried dolomitization. This study can provide a specific sample for microbial induced lacustrine dolomite precipitation in ancient strata and reference for exploration in the study area.
- Bohai Bay basin,
- Huanghekou sag,
- Shahejie Formation,
- dolomite origin,
- microbial dolomite,
- buried dolomitization,
- sedimentation

FullText(HTML)

References(65)

References

Berner, R.A., 1980.Early Diagenesis: A Theoretical Approach. Princeton University Press, New Jersey.

Bontognali, T.R.R., Vasconcelos, C., Warthmann, R.J., et al., 2010. Dolomite Formation within Microbial Mats in the Coastal Sabkha of Abu Dhabi (United Arab Emirates). Sedimentology, 57(3): 824-844. https://doi.org/10.1111/j.1365-3091.2009.01121.x

Bosak, T., Souza-Egipsy, V., Corsetti, F.A., et al., 2004. Micrometer-Scale Porosity as a Biosignature in Carbonate Crusts. Geology, 32(9): 781-784. https://doi.org/10.1130/g20681.1

Brooks, G.R., Doyle, L.J., Suthard, B.C., et al., 2003. Facies Architecture of the Mixed Carbonate/Siliciclastic Inner Continental Shelf of West-Central Florida: Implications for Holocene Barrier Development. Marine Geology, 200(1-4): 325-349. https://doi.org/10.1016/S0025-3227(03)00190-7

Dai, C.C., Zheng, R.C., Wen, H.G., et al., 2008.Origin of Lacustrine Dolomite in the Paleogene Shahejie Formation of Liaodongwan Basin, China. Journal of Chengdu University of Technology (Science & Technology Edition), 35(2): 187-193(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb200802014

Dong, G.Y., Chen, H.D., He, Y.B., et al., 2007. Some Problems on the Study of the Mixed Siliciclastic-Carbonate Sediments. Advances in Earth Science, 22(9): 931-939(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkxjz200709007

Gao, G., Yang, S.R., Qu, T., 2018. Research Status of Mixing Sediments and Their Relationship with Petroleum Enrichment. Geological Science and Technology Information, 37(6):82-88(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201806010

García-Hidalgo, J.F., Gil, J.G., Segura, M., et al., 2007. Internal Anatomy of a Mixed Siliciclastic-Carbonate Platform: The Late Cenomanian-Mid Turonian at the Southern Margin of the Spanish Central System. Sedimentology, 54(6): 1245-1271. https://doi.org/10.1111/j.1365-3091.2007.00880.x

Huo, S.J., Yang, X.H., Wang, Q.B., et al., 2015. Controlling Factors on Diamictite Reservoir in Shahejie Formation, H-1 Structure, Huanghekou Depression. Geoscience, 29 (6): 1348-1359 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201506009

Keith, M.L., Weber, J.N., 1964. Carbon and Oxygen Isotopic Composition of Selected Limestones and Fossils. Geochimica et Cosmochimica Acta, 28(10-11): 1787-1816. https://doi.org/10.1016/0016-7037(64)90022-5

Krause, S., Liebetrau, V., Gorb, S.N., et al., 2012. Microbial Nucleation of Mg-Rich Dolomite in Exopolymeric Substances under Anoxic Modern Seawater Salinity: New Insight into an Old Enigma. Geology, 40(7): 587-590. https://doi.org/10.1130/G32923.1

Li, D.S., 1981. Geological Structure and Hydrocarbon Occurrence of Bohai Gulf Oil and Gas Basin (China). Marine Geological Research, 1(1):3-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ198101001.htm

Li, J.Y., Wan, C.F., Fan, T.Z., 1991. Weathering Crust of Carbonate Rocks and Process of Karst Earth Formation. Carsologica Sinica, 10(1): 29-38(in Chinese with English abstract).

Liao, J., Dong, Z.X., Zhai, G.Y., et al., 2008. Feature of Oligocene Shahejie Lower-lst Member Lacustrine Dolostone in Qikou Depression, Bohaiwan Basin, and Difference of It from Marine Dolostone. Marine Origin Petroleum Geology, 13(1): 18-24(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HXYQ200801005.htm

Liu, S.L., Wang, Q.F., Gong, Y.J., et al., 2012. Paleogene Microfossil Assemblages from the Bohai Area and Their Importance for the Oil and Gas Exploration. Journal of Stratigraphy, 36(4): 700-709(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ201204004.htm

Mount, J.F., 1984. Mixing of Siliciclastic and Carbonate Sediments in Shallow Shelf Environments. Geology, 12(7): 432-435. https://doi.org/10.1130/0091-7613(1984)12432:MOSACS > 2.0.CO; 2 doi: 10.1130/0091-7613(1984)12432:MOSACS>2.0.CO;2

Pan, W.J., Wang, Q.B., Liu, S.L., et al., 2017.Origin of Lacustrine Bioclastic Dolostone in the Paleogene Shahejie Formation: A Case Study in Shijiutuo Area, Bohai Sea. Journal of Palaeogeography, 19(5): 835-848(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX201705008.htm

Perri, E., Tucker, M.E., 2007. Bacterial Fossils and Microbial Dolomite in Triassic Stromatolites. Geology, 35(3): 207-210. https://doi.org/10.1130/G23354A.1

Qu, C.W., Lin, C.M., Cai, M.J., et al., 2014. Characteristics of Dolostone Reservoir in Sha 3 Group from Palaeogene Shahejie Formation in Beitang Sag, Bohaiwan Basin. Acta Geologica Sinica, 88(8): 1588-1602(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201408019

Sánchez-Román, M., Vasconcelos, C., Schmid, T., et al., 2008. Aerobic Microbial Dolomite at the Nanometer Scale: Implications for the Geologic Record. Geology, 36(11): 879-882. https://doi.org/10.1130/G25013A.1

Song, B.R., Han, H.D., Cui, X.D., et al., 2015. Petrogenesis Analysis of Lacustrine Analcite Dolostone of the Member 4 of Paleogene Shahejie Formation in Liaohe Depression, Bohai Bay Basin. Journal of Palaeogeography, 17(1): 33-44(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201501004

Tang, L.J., Wan, G.M., Zhou, X.H., et al., 2008. Cenozoic Geotectonic Evolution of the Bohai Basin. Geological Journal of China Universities, 14(2):191-198 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200802008

Tian, J.C., Yin, G., Qin, J.X., et al., 1998. The Relationship between the Transgression of Eogene and the Origin of Lacustrine Dolomitite in Eastern China-Taking the Shahejie Formation of Dongying Sag as Example. China Offshore Oil and Gas (Geology), 12(4): 34-38 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD199804008.htm

van Lith, Y., Warthmann, R., Vasconcelos, C., et al., 2003. Sulphate‐Reducing Bacteria Induce Low‐Temperature Ca‐Dolomite and High Mg‐Calcite Formation. Geobiology, 1(1): 71-79. https://doi.org/10.1046/j.1472-4669.2003.00003.x

Vasconcelos, C., McKenzie, J.A., Bernasconi, S.M., et al., 1995. Microbial Mediation as a Possible Mechanism for Natural Dolomite Formation at Low Temperatures. Nature, 377(6546): 220-222. https://doi.org/10.1038/377220a0

Wang, B.J., Cai, M.J., Lin, C.M., et al., 2014. Characteristics and Origin of Lacustrine Dolostone of the Paleogene Shahejie Formation in Tanggu area, Bohai Bay Basin. Journal of Palaeogeography, 16(1): 65-76 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201401007

Wang, G.Z., 2001.Mixed Sedimentation of Recent Reefoid Carbonates and Terrigenous Clastics in the North Continental Shelf of the South China Sea. Journal of Palaeogeography, 3(2): 47-54(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb200102007

Wang, J.Q., Liu, B., Luo, P., et al., 2014. Classification and Genesis of Sinian Mixosedimentite from Northwest Margin of Tarim Basin, China. Journal of Chengdu University of Technology (Science & Technology Edition), 41(3): 339-346 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb201403010

Wang, Q.B., Liu, L., Niu, C.M., et al., 2018. Impacts of the Freshwater Diagenetic Environment to the Mix-Deposition of Lacustrine Carbonate and Clastic at the Steep Slope of Shijiutuo Uplift, Bohai Bay Basin. Earth Science, (Suppl.2): 234-242(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX2018S2019.htm

Wang, Q.B., Liu, L., Niu, C.M., et al., 2019. The Geological Evidences and Impacts of Deep Thermal Fluid on Lacustrine Carbonate Reservoir in the Actic Area of the North Part of Bozhong Depression, Bohai Bay Basin. Earth Science, 44(8): 2751-2760 (in Chinese with English abstract).

Wang, X.L., Chou, I.M., Hua, W.X., et al., 2016. Kinetic Inhibition of Dolomite Precipitation: Insights from Raman Spectroscopy of Mg²⁺-SO₄^2- Ion Pairing in MgSO₄/MgCl₂/NaCl Solutions at Temperatures of 25 to 200 ℃. Chemical Geology, 435(2016): 10-21. https://doi.org/10.1016/j.chemgeo.2016.04.020

Warthmann, R., van Lith, Y., Vasconcelos, C., et al., 2000. Bacterially Induced Dolomite Precipitation in Anoxic Culture Experiments. Geology, 28(12): 1091-1094. https://doi.org/10.1130/0091-7613(2000)0281091:bidpia > 2.3.co; 2 doi: 10.1130/0091-7613(2000)0281091:bidpia>2.3.co;2

Xie, X.N., Ye, M.S., Xu, C.G., et al., 2018. High Quality Reservoirs Characteristics and Forming Mechanisms of Mixed Siliciclastic-Carbonate Sediments in the Bozhong Sag, Bohai Bay Basin. Earth Science, 43 (10): 3526-3539(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201810015

Yang, C.Q., Sha, Q.A., 1990. Sedimentary Environment of the Middle Devonian Qujing Formation, Qujing, Yunnan Province: A Kind of Mixing Sedimentation of Terrigenous Clastics and Carbonate. Acta Sedimentologica Sinica, 8(2): 59-66(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB199002008.htm

Zhang, F., Xu, H.F., Konishi, H., et al., 2012. Polysaccharide-Catalyzed Nucleation and Growth of Disordered Dolomite: A Potential Precursor of Sedimentary Dolomite. American Mineralogist, 97(4): 556-567. https://doi.org/10.2138/am.2012.3979

Zhang, J.T., He, Z.L., Yue, X.J., et al., 2017. Genesis of Iron-Rich Dolostones in the 5th Member of the Majiagou Formation of the Ordovician in Ordos Basin. Oil & Gas Geology, 38(4): 776-783(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201704014

Zhang, X.H., 2000. Classification and Origin of Mixosedimentite. Geological Science and Technology Information, 19(4): 31-34(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200004006

Zhao, K., Song, Z.Q., Du, X.B., et al., 2018. Dolomitization Genetic Mechanism of Carbonate-Siliciclastic Mixed Rock Reservoir in CFD-A Tectonic Belt, Bohai Sea. Petroleum Geology & Experiment, 40(2): 218-225(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sysydz201802012

Zhao, W.Z., Shen, A.J., Qiao, Z.F., et al., 2018. The Genetic Types and Distinguished Characteristics of Dolostone and the Origin of Dolostone Reservoirs. Petroleum Exploration and Development, 45(6): 923-935(in Chinese with English abstract). http://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFD&filename=PEAD201806002

Zhu, W.L., 2009. Paleolimnology and Source Rock Studies of Cenozoic Hydrocarbon-Bearing Offshore Basins in China. Geological Publishing House, Beijing (in Chinese).

戴朝成, 郑荣才, 文华国, 等, 2008.辽东湾盆地沙河街组湖相白云岩成因研究.成都理工大学学报(自然科学版), 35(2): 187-193. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb200802014

董桂玉, 陈洪德, 何幼斌, 等, 2007.陆源碎屑与碳酸盐混合沉积研究中的几点思考.地球科学进展, 22(9): 931-939. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkxjz200709007

高岗, 杨尚儒, 屈童, 2018.混合沉积研究现状及其与油气富集的关系.地质科技情报, 37(6): 82-88. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201806010

霍沈君, 杨香华, 王清斌, 等, 2015.黄河口凹陷H-1构造沙河街组混积岩储层控制因素.现代地质, 29(6): 1348-1359. http://d.wanfangdata.com.cn/Periodical/xddz201506009

李德生, 1981.渤海湾含油气盆地的地质构造特征与油气田分布规律.海洋地质研究, 1(1): 3-20. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ198101001.htm

李景阳, 王朝富, 樊廷章, 1991.试论碳酸盐岩风化壳与喀斯特成土作用.中国岩溶, 10(1): 29-38. http://www.cnki.com.cn/Article/CJFDTotal-ZGYR199101004.htm

廖静, 董兆雄, 翟桂云, 等, 2008.渤海湾盆地歧口凹陷沙河街组一段下亚段湖相白云岩及其与海相白云岩的差异.海相油气地质, 13(1): 18-24. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hxyqdz200801004

刘士磊, 王启飞, 龚莹杰, 等, 2012.渤海海域古近纪微体化石组合特征及油气勘探意义.地层学杂志, 36(4): 700-709. http://www.cnki.com.cn/Article/CJFDTotal-DCXZ201204004.htm

潘文静, 王清斌, 刘士磊, 等, 2017.渤海海域石臼坨地区古近系沙河街组湖相生屑白云岩成因.古地理学报, 19(5): 835-848. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201705006

曲长伟, 林春明, 蔡明俊, 等, 2014.渤海湾盆地北塘凹陷古近系沙河街组三段白云岩储层特征.地质学报, 88(8): 1588-1602. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201408019

宋柏荣, 韩洪斗, 崔向东, 等, 2015.渤海湾盆地辽河坳陷古近系沙河街组四段湖相方沸石白云岩成因分析.古地理学报, 17(1): 33-44. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201501004

汤良杰, 万桂梅, 周心怀, 等, 2008.渤海盆地新生代构造演化特征.高校地质学报, 14(2): 191-198. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200802008

田景春, 尹观, 覃建雄, 等, 1998.中国东部早第三纪海侵与湖相白云岩成因之关系--以东营凹陷沙河街组为例.中国海上油气(地质), 12 (04): 34-38. http://www.cnki.com.cn/Article/CJFDTotal-ZHSD199804008.htm

王兵杰, 蔡明俊, 林春明, 等, 2014.渤海湾盆地塘沽地区古近系沙河街组湖相白云岩特征及成因.古地理学报, 16(1): 65-76. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201401007

王国忠, 2001.南海北部大陆架现代礁源碳酸盐与陆源碎屑的混合沉积作用.古地理学报, 3(2): 47-54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb200102007

王杰琼, 刘波, 罗平, 等, 2014.塔里木盆地西北缘震旦系混积岩类型及成因.成都理工大学学报(自然科学版), 41(3): 339-346. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb201403010

王清斌, 刘立, 牛成民, 等, 2018.石臼坨凸起陡坡带大气淡水成岩环境对湖相混积岩储层的影响.地球科学, (增刊2): 234-242. doi: 10.3799/dqkx.2018.138

王清斌, 刘立, 牛成民, 等, 2019.渤中凹陷北部陡坡带热液活动及其对湖相碳酸盐岩储层的影响.地球科学, 44(8): 2751-2760. doi: 10.3799/dqkx.2018.347

解习农, 叶茂松, 徐长贵, 等, 2018.渤海湾盆地渤中凹陷混积岩优质储层特征及成因机理.地球科学, 43(10): 3526-3539. doi: 10.3799/dqkx.2018.277

杨朝青, 沙庆安, 1990.云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳.沉积学报, 8(2): 59-66. http://www.cqvip.com/QK/95994X/19902/221837.html

张军涛, 何治亮, 岳小娟, 等, 2017.鄂尔多斯盆地奥陶系马家沟组五段富铁白云石成因.石油与天然气地质, 38(4): 776-783. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201704014

张雄华, 2000.混积岩的分类和成因.地质科技情报, 19(4): 31-34. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200004006

赵珂, 宋章强, 杜学斌, 等, 2018.渤海海域曹妃甸A构造带混积岩储层白云岩化成因机理分析.石油实验地质, 40(2): 218-225. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sysydz201802012

赵文智, 沈安江, 乔占峰, 等, 2018.白云岩成因类型、识别特征及储集空间成因.石油勘探与开发, 45(6): 923-935. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syktykf201806002

朱伟林, 2009.中国近海新生代含油气盆地古湖泊学与烃源条件.北京:地质出版社.

Relative Articles

Supplements(0)

Cited By

Proportional views