吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (2): 355-369.doi: 10.13278/j.cnki.jjuese.201702103

• 地质与资源 • 上一篇    下一篇

白云岩化作用类型及机理——以歧口凹陷古近系沙河街组一段为例

高福红1, 张永胜1, 蒲秀刚2, 杨杨3, 张鐘月4   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 大港油田勘探开发研究院, 天津 300280;
    3. 长春工程学院勘查与测绘工程学院, 长春 130021;
    4. 辽宁省地震局, 沈阳 110034
  • 收稿日期:2016-06-25 出版日期:2017-03-26 发布日期:2017-03-26
  • 作者简介:高福红(1963),女,教授,博士生导师,主要从事岩石学方面的研究,E-mail:gaofh@jlu.edu.cn
  • 基金资助:
    国家自然科学基金项目（41502145）；吉林省教育厅"十三五"科学技术研究规划项目（2016-0313）

Type of Dolomization and Formation Mechanism: A Case Study of Palaeogene Es1 in Qikou Sag

Gao Fuhong1, Zhang Yongsheng1, Pu Xiugang2, Yang Yang3, Zhang Zhongyue4   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Research Institute of Exploration and Development, Dagang Oilfield Company, PetroChina, Tianjin 300280, China;
    3. School of Prospecting & Surveying Engineering, Changchun Institute of Technology, Changchun 130021, China;
    4. Earthquake Administration of Liaoning Province, Shenyang 110034, China
  • Received:2016-06-25 Online:2017-03-26 Published:2017-03-26
  • Supported by:
    Supported by the National Natural Science Foundation of China(41502145)and Science and Technology Research Program of the 13th Five-Year from Education Department of Jilin Province(2016-0313)

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摘要： 通过镜下鉴定和地球化学分析对歧口凹陷古近系沙一段白云岩进行了研究，综合分析了研究区发育的岩石类型及其成因。结果表明：研究区发育泥-微晶白云岩、灰质白云岩、白云质灰岩及少量颗粒白云岩；Sr/Ba值为0.4~4.9，V/Ni值为1.3~7.1，Z值（盐度指数）分布在122.6~162.5；87Sr/86Sr值和同期海水极为接近，因此推断湖盆遭受了海侵作用，海侵为白云岩化作用提供了Mg2+；有序度分布在0.22~0.53，整体较低；Mg/Ca值为0.73~0.91，反映了富钙低镁的特征，表明白云岩形成于准同生阶段。碳氧同位素分析表明，研究区白云岩形成于浅埋藏环境，并且受到了发酵作用的影响，异常高的Sr值也反映了微生物活动的存在。通过以上证据推断本区白云岩是在准同生期、浅埋藏环境、经渗透回流作用形成的，并且受到了发酵作用的影响。

关键词: 古近系, 白云岩化, 碳氧同位素, 歧口凹陷

Abstract: In terms of the microscopic identification and geochemical analysis, study has been made on the dolostones of Palaeogene Es1 in Qikou sag. The result shows that there are microcrystalline-micritic dolomite, calcite dolomite, dolomite limestone, and a little grain dolomite. Sr/Ba ratio is from 0.4 to 4.9, V/Ni ratio is from 1.3 to 7.1, Z value distributed between 122.6~162.5, 87Sr/86Sr ratio of dolostone is extremely close to the seawater. According to the mentioned values, the lake basin was influenced by transgression activity, which brought a large number of Mg2+ for dolomization. The order degree of dolomite is between 0.22-0.53, Mg/Ca ratio is between 0.73-0.91, it has characteristics of rich in Ca2+ and poor in Mg2+, which indicates that the dolostone was formed during the penecontemporaneous period. Carbon and oxygen isotope analysis implies that the dolostone was formed in shallow burial environment, the extremely positive δ13C anomaly indicates that the process of dolomization was affected by fermentation, the abnormal high Sr value suggests an activity of bacteria. Based on the analysis above, the dolostone was formed in shallow burial environment during the penecontemporaneous period by the process of seepage-reflux and the process was affected by methanation.

Key words: Palaeogene, dolomization, carbon and oxygen isotopes, Qikou sag

中图分类号: 

  • P581
[1] Zengler D H, Dunham J D, Ethington R L. Concepts and Models of Dolomitization[J]. Earth-Science Reviews, 1979, 17(3):285-286.
[2] Sun S Q. Dolomite Reservoirs:Porosity Evolution and Reservoir Characteristics[J]. American Association of Petroleum Geologists Bulletin, 1995,79(2):186-204.
[3] 于亚苹,刘立,徐守立,等. 西沙群岛西科1井梅山组一段储层物性特征及储集评价[J]. 世界地质,2015, 34(4):1069-1078. Yu Yaping, Liu Li, Xu Shouli. et al. Reservoir Characteristics and Evaluation of the First Member of Meishan Formation in Well Xike 1,Xisha Islands[J]. Global Geology,2015,34(4):1069-1078.
[4] Land L S. Failure to Precipitate Dolomite at 25℃ from Dilute Solution Despite 1000 Fold Oversaturation After 32 Years[J]. Aquatic Geochemistry, 1998,4(3):361-368.
[5] Mckenzie J A, Vasconcelos C. Dolomite Mountains and the Origin of the Dolomite Rock of Which They Mainly Consist:Historical Developments and New Perspectives[J]. Sedimentology, 2009, 56(1):205-219.
[6] Adams J E, Rhodes M L. Dolomitization by Seepage Refluxion[J]. American Association of Petroleum Geologists Bulletin,1960,44(12):1912-1920.
[7] Jinghwa Hsü K, Siegenthaler C. Preliminary Experi-ments on Hydrodynamic Movement Induced by Evaporation and Their Bearing on the Dolomite Problem[J]. Sedimentology,1969,12(1/2):11-25.
[8] Illing L V. Deposition and Diagenesis of Some Upper Paleozoic Carbonate Sediments in Western Canada[C]//Proceedings of the Fifth World Petroleum Congress. New York:[s.n.],1959:23-52.
[9] Badiozamani K. The Dorag Dolomitization Model:App-lication to the Middle Ordovician of Wisconsin[J]. Jour Sediment Petrol,1973,43(4):965-984.
[10] 蒲秀刚,周立宏,肖敦清,等. 黄骅坳陷歧口凹陷西南缘湖相碳酸盐岩地质特征[J].石油勘探与开发,2011,38(2):136-144. Pu Xiugang, Zhou Lihong, Xiao Dunqing, et al. Lacustrine Carbonates in the Southwest Margin of Qikou Sag, Huanghua Depression, Bohai Bay Basin[J]. Petroleum Exploration and Development,2011,38(2):136-144.
[11] 廖静,董兆雄,翟桂云,等. 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[J]. 海相油气地质,2008,13(1):18-24. Liao Jing, Dong Zhaoxiong, Zhai Guiyun, et al. Featureof Oligocene Shahejie Lower-1st Member Lacustrine Dolostone in Qikou Depression, Bohaiwan Basin, and Difference of It from Marine Dolostone[J]. Marine Origin Petroleum Geology, 2008,13(1):18-24.
[12] 黄鹏,李雪,郭瑞. 歧口凹陷沙一下亚段湖相白云岩岩石学特征及成因分析[J]. 科技导报,2014,32(2):50-56. Huang Peng, Li Xue, Guo Rui. Research on Petrologic Character and Genetic Mode of Lacustrine Dolomite[J]. Science & Technology Review,2014,32(2):50-56.
[13] 张江江,黄鹏,冯学谦,等. 歧口凹陷沙一下亚段白云岩储集空间特征研究[J]. 科技导报,2011,29(17):39-44. Zhang Jiangjiang, Huang Peng, Feng Xueqian, et al. Analysis of Reservoir Space Characteristics of Dolomite Reservoirs in Sha 1 Lower Sub-Interval in Qikou Depression[J]. Science & Technology Review,2011,29(17):39-44.
[14] 杨扬,高福红,蒲秀刚. 歧口凹陷古近系沙河街组白云岩稀土元素特征及成因[J]. 中国石油大学学报(自然科学版),2014,38(2):1-9. Yang Yang, Gao Fuhong, Pu Xiugang. REE Characteristics and Genesis of Dolostones from Paleogene Shahejie Formation in Qikou Depression[J]. Journal of China University of Petroleum (Edition of Natural Science),2014,38(2):1-9.
[15] 李绍光,吴涛,方文娟,等. 中国石油地质志:卷四:大港油田[M]. 北京:石油工业出版社,1991:74-113. Li Shaoguang, Wu Tao, Fang Wenjuan, et al. Petroleum Geology of China:Volume 4:Dagang Oilfield[M]. Beijing:Prtroleum Industry Press,1991:74-113.
[16] 马伯永,王根厚,李尚林,等. 羌塘盆地东部中侏罗统陆源碎屑与碳酸盐混合沉积成岩特征[J]. 吉林大学学报(地球科学版),2015,45(5):1310-1321. Ma Boyong, Wang Genhou, Li Shanglin, et al. Characteristics of Mixed Sedimentation and Diagenesis of Terrigenous Clastic Rock and Carbonate:The Middle Jurassic in the East Qiangtang Basin, Tibet, China[J]. Journal of Jilin University(Earth Science Edition),2015,45(5):1310-1321.
[17] 曾理,万茂霞,彭英. 白云石有序度及其在石油地质中的应用[J]. 天然气勘探与开发,2004,27(4):64-66,72. Zeng Li, Wan Maoxia, Peng Ying. Dolomite Sequentiality and Its Application to Petroleum Geology[J].Natural Gas Exploration and Development,2004,27(4):64-66,72.
[18] 李亚林,黄永建,王成善,等. 西藏措勤盆地白垩系白云岩地球化学特征及其成因分析[J].岩石学报,2008,24(3):609-615. Li Yalin, Huang Yongjian, Wang Chengshan, et al. Geochemical Characteristics and Genetic Analysis of the Cretaceous Dolomite in the Cuoqin Basin, Qinghai-Tibet Plateau[J]. Acta Petrologica Sinica,2008,24(3):609-615.
[19] 袁剑英,黄成刚,曹正林,等. 咸化湖盆白云岩碳氧同位素特征及古环境意义:以柴西地区始新统下干柴沟组为例[J]. 地球化学,2015,44(3):254-266. Yuan Jianying, Huang Chenggang, Cao Zhenglin, et al. Carbon and Oxygen Isotopic Composition of Saline Lacustrine Dolomite and Its Palaeoenvironmental Significance:A Case Study of Lowereocene Ganchaigou Formation in Western Qaidam Basin[J]. Geochimica,2015,44(3):254-266.
[20] Kelts K, Talbot M. Lacustrine Carbonates as Geoche-mical Archives of Environmental Change and Biotic/Abiotic Interactions[M]//Large Lakes. Berlin:Springer,1990:288-315.
[21] Keith M L, Weber J N. Carbon and Oxygen Isotopic Composition of Selected Limestones and Fossils[J]. Geochim Cosmochim Acta,1964,28(10/11):1787-1816.
[22] 夏文杰,李秀华. 青海小柴旦盐湖湖滩岩中原生白云石的发现及其意义[J]. 沉积学报,1986,4(2):19-25,134. Xia Wenjie, Li Xiuhua. The Discovery of Primary Dolomite from Beach Rock in the Xiaochaidan Salt Lake of Qinghai and Its Significance[J]. 1986,4(2):19-25,134.
[23] 田永净,马永生,刘波,等. 川东北元坝气田长兴组白云岩成因研究[J]. 岩石学报,2014,30(9):2766-2776. Tian Yongjing, Ma Yongsheng, Liu Bo,et al. Dolomitization of the Upper Permian Changxing Formation in Yuanba Gas Field, NE Sichuan Basin, China[J]. Acta Petrologica Sinica,2014,30(9):2766-2776.
[24] Ján Veizer, Davin Ala, Karem Azmy, et al. 87Sr/86Sr, δ13C, δ18O Evolution of Phanerozoic Seawater[J]. Chemical Geology,1999,161(1/2/3/4/5/6):59-88.
[25] 任来义,林桂芳,谈玉明,等.从古生物和地球化学标志看东濮凹陷早第三纪的海侵事件[J]. 西安石油学院学报(自然科学版),2002,17(1):20-23. Ren Laiyi, Lin Guifang, Tan Yuming,et al. Studying Marine Transgression of Early Tertiary in Dongpu Depression from Paleontologic and Geochemical Marks[J]. Journal of Xi'an Petroleuminstitute(Natural Science Edition),2002,17(1):20-23.
[26] Yang J D, Sun W G, Wang Z Z, et al. Variations in Sr and C Isotopes and Ce Anomalies Insuccessions from China:Evidence for the Oxygenation of Neoproterozoic Seawater[J]. Precambrian Reseach,1999,93(2/3):215-233.
[27] 胡忠贵,郑荣才,文华国,等. 川东邻水-渝北地区石炭系黄龙组白云岩成因[J]. 岩石学报,2008,24(6):1369-1378. Hu Zhonggui, Zheng Rongcai, Wen Huaguo,et al. Dolostone Genesis of Huanglong Formation of Carboniferous in Linshui of Eastern Sichuan-Northern Chongqing Area[J]. Acta Petrologica Sinica, 2008,24(6):1369-1378.
[28] 杨威,王清华,刘效曾. 塔里木盆地和田河气田下奥陶统白云岩成因[J]. 沉积学报,2000,18(4):544-548. Yang Wei, Wang Qinghua, Liu Xiaozeng. Dolomite Origin of Lower Ordovician in Hetian Rivergas Field Tarim Basin[J]. Acta Sedimentologica Sinica, 2000,18(4):544-548.
[29] 邵龙义,何宏,彭苏萍,等. 塔里木盆地巴楚隆起寒武系及奥陶系白云岩类型及形成机理[J]. 古地理学报,2002,4(2):19-30. Shao Longyi, He Hong, Peng Suping,et al. Types and Origin of Dolostones of the Cambrian and Ordovician of Bachu Uplift Area in Tarim Basin[J]. Journal of Palaeogeography,2002,4(2):19-30.
[30] McArthur J M,Kennedy W J, Gale A S, et al. St-rontium Isotope Stratigraphy of the Late Cretaceous:Intercontinental Correlation of the Campanian-Maastrichian Boundary[J]. Terra Nova, 1992, 4(4):385-395.
[31] 陈世悦,李聪,杨勇强,等. 黄骅坳陷歧口凹陷沙一下亚段湖相白云岩形成环境[J]. 地质学报,2012,86(10):1679-1687. Chen Shiyue, Li Cong, Yang Yongqiang, et al. Deposition Environment of the Lacustrine Dolomite in Sha-1 Lower Submember of the Qikou Sag, Huanghua Depression[J]. Acta Geologica Sinica,2012, 86(10):1679-1687.
[32] 张云孝, 李向东, 张冀. 西天山喀拉达拉基性岩体及其构造背景[J]. 新疆地质,2000,18(3):258-263. Zhang Yunxiao, Li Xiangdong, Zhang Ji.Basic Pluton and Its Tectonic Setting in Kaladala of West Tianshan Mountains, China[J]. Xinjiang Geology,2000,18(3):258-263.
[33] 杨浩.东天山地区花岗岩的成因、特征、分布规律及其与构造背影和成矿关系[D].南京:南京大学,1988. Yang Hao.The Genesis, Characteristics, Distribution Rule of the Granite in the Eastern Tianshan Mountain and It's Relation to Tectonic Background and Ore Deposit[D]. Nanjing:Nanjing University,1988.
[34] 田景春, 尹观,覃建雄,等. 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[J]. 中国海上油气:地质,1998,12(4):250-254. Tian Jingchun, Yin Guan, Qin Jianxiong, et al. The Relatioin Between the Transgression of Eogene and the Origin of Lacustrine Dolomitite in Eastern China:Taking the Shahejie Formation of Dongying Sag as Example[J]. China Offshore Oil and Gas:Geology,1998,12(4):250-254.
[35] Machel H G, Mountjoy E W. Chemistry and Envi-ronments of Dolomitization:A Reappraisal[J]. Earth Science Reviews,1986,23(3):175-222.
[36] Li H C,Ku T L. δ13C-δ18O Covariance as a Palaeohydrological Indicator for Closed-Basin Lakes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,1997,133(1/2):69-80.
[37] Hudson J D. Stable Isotopes and Limestone Lithi-fication[J]. Journal of the Geological Society of London,1977,133:637-660.
[38] Coleman M L, Berner R A, Durand B, et al. Geo-chemistry of Diagenetic Non-Silicate Minerals Kinetic Considerations[J]. Philosophical Transactions of the Royal Society of London,1985,315:39-56.
[39] Pirrie D, Marshall J D. Field Relationships and Stable Isotope Geochemistry of Concretions from James Ross Island, Antarctica[J]. Sedimentary Geology,1991,71(3/4):137-150.
[40] Nelson C S, Smith A M. Stable Oxygen and Carbon Isotope Compositional Fields for Skeletal and Diagenetic Components in New Zealand Cenozoic Nontropical Carbonate Sediments and Limestones:A Synthesis and Review[J]. New Zealand Journal of Geology and Geophysics,1996,39(1):93-107.
[41] Curtis C D, Petrowski C, Oertel G. Stable Carbon Isotope Ratios Within Carbonate Concretions:A Clue to Place and Time of Formation[J]. Nature,1972,235:98-100.
[42] Irwin H, Curtis C, Coleman M. Isotopic Evidence for Source of Diagenetic Carbonates Formed During Burial of Organic-Rich Sediments[J]. Nature,1977,269:209-213.
[43] 伊海生,林金辉,周恳恳,等. 青藏高原北部新生代湖相碳酸盐岩碳氧同位素特征及古环境意义[J]. 古地理学报,2007,9(3):303-312. Yi Haisheng, Lin Jinhui, Zhou Kenken,et al. Carbon and Oxygen Isotope Characteristics and Palaeoenvionmental Implication of the Cenozoic Lacustrine Carbonate Rocks in Northern Qinghai Tibetan Plateau[J]. Journal of Palaeogeography, 2007,9(3):303-312.
[44] 覃建雄,曾允孚. 鄂尔多斯盆地东部下奥陶统白云岩地球化学研究[J]. 矿物学报,1994,14(1):22-31. Qin Jianxiong, Zeng Yunfu. Geochemistryof Lower Ordovician Dolostones in Eastern Ordos Basin[J]. Acta Mineralogeca Sinica,1994,14(1):22-31.
[45] Sánchez-Román M, Mckenzie J A, Wagener A D L R, et al. Experimentally Determined Biomediated Sr Partition Coefficient for Dolomite:Significance and Implication for Natural Dolomite[J].Geochimica Et Cosmochimica Acta,2011,75(3):887-904.
[46] Talbot M R, Kelts K. Paleolimnological Signatures from Carbon and Oxygen Isotopic Ratios in Carbonates from Organic-Rich Lacustrine Sediments:Chapter 6[J]. AAPG Memoir,1990,50:99-112.
[47] 王兵杰,蔡明俊,林春明,等. 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[J]. 古地理学报,2014,16(1):65-76. Wang Bingjie, Cai Mingjun, Lin Chunming, et al. Characteristics and Origin of Lacustrine Dolostone of the Paleogene Shahejie Formation in Tanggu Area, Bohai Baybasin[J]. Journal of Palaeogeography,2014,16(1):65-76.
[48] 李得立, 谭先锋, 夏敏全,等. 东营凹陷沙四段湖相白云岩沉积特征及成因[J]. 断块油气田, 2010,17(4):418-422. Li Deli, Tan Xianfeng, Xia Minquan, et al. Sedimentary Characteristicand Genesis of Lacustrine Dolomite in the Fourth Member of Shahejie Formation in Dongying Sag[J]. Fault-Block oil and Gas Field,2010,17(4):418-422.
[49] 戴朝成, 郑荣才, 文华国,等. 辽东湾盆地沙河街组湖相白云岩成因研究[J]. 成都理工大学学报(自然科学版),2008,35(2):187-193. Dai Chaocheng, Zheng Rongcai, Wen Huaguo, et al. Origin of Lacustrine Dolomite in the Paleogene Shahejie Formation of Liaodongwan Basin China[J].Journal of Chengdu University of Technology (Science Technology Editon),2008,35(2):187-193.
[50] 何莹, 鲍志东, 沈安江,等. 塔里木盆地牙哈英买力地区寒武系-下奥陶统白云岩形成机理[J]. 沉积学报, 2006, 24(6):806-818. He Ying, Bao Zhidong, Shen Anjiang, et al. The Genetic Mechanismof Dolostones of the Cambrian Lower Ordovician in Yaha Yingmaili Region Tarim Basin[J]. Acta Sedimentologica Sinica,2006,24(6):806-818.
[51] 赵澄林.沉积岩石学[M].北京:石油工业出版社,2001:311-324. Zhao Chenglin.Sedimentary Petrology[M].Beijing:Petroleum Industry Press,2001:311-324.
[52] 梅洪明, 汪品先. 湖泊原生碳酸盐化学沉积模型及其应用[J]. 同济大学学报(自然科学版),1997,25(5):565-569. Mei Hongming, Wang Pinxian. Modelfor Chemical Sedimentation of Primarylake Carbonates and Its Application[J]. Journal of Tongji University(Natural Science),1997,25(5):565-569.
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