Advanced Search
Volume 44 Issue 4
Jul.  2022
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2022  >  44(4): 593-602
LI Miao, ZHOU Yushuang, ZHAO Yongqiang, GENG Feng, QIAO Guilin, HAO Jianlong. Geochemical characteristics and fluid origins of fracture- and cave-filling calcites of Ordovician in Yubei area, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(4): 593-602. doi: 10.11781/sysydz202204593
Citation: LI Miao, ZHOU Yushuang, ZHAO Yongqiang, GENG Feng, QIAO Guilin, HAO Jianlong. Geochemical characteristics and fluid origins of fracture- and cave-filling calcites of Ordovician in Yubei area, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(4): 593-602. doi: 10.11781/sysydz202204593
shu

Geochemical characteristics and fluid origins of fracture- and cave-filling calcites of Ordovician in Yubei area, Tarim Basin

doi: 10.11781/sysydz202204593
  • 1.

    Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • 2.

    Research Institute of Exploration and Production, Northwest Oilfield Company, SINOPEC, Urumqi, Xinjiang 830011, China

  • Received Date: 2021-05-10
  • Rev Recd Date: 2022-05-20
  • Publish Date: 2022-07-28
    Abstract
  • The genesis of carbonate reservoirs of the Lower-Middle Ordovician strata has been an important topic for petroleum exploration in the Yubei area, Tarim Basin. To investigate the stages and properties of paleo-fluid and discuss the reservoir origin, the geochemical and cathodoluminescence features of the Ordovician fracture- and cave-filling calcites from wells in the Yubei area were analyzed combining with the regional tectonic background. Results show that the REE distribution patterns and occurrences of samples from different wells have the characteristics of seawater and fresh water, respectively. The average values of Sr isotopes gradually decrease from east to west. Moreover, the average value of 87Sr/86Sr in high-angle fracture calcites is higher than those of cave-filling and horizontal-fracture calcites, suggesting obvious variations of fluid properties in different regions and sample occurrences. Therefore, the diagenetic environment of the Lower-Middle Ordovician carbonates in the Yubei area may be open. The decreases of meteoric alteration from east to west can be attributed to the Middle Caledonian and Early Hercynian tectonic setting. Moreover, the progress of reservoir modification by fluids is mainly affected by fault activity intensity.

     

    • FullText(HTML)
  • loading
    • References(43)
  • [1]
    钱一雄, 余腾孝, 周凌方, 等. 麦盖提斜坡东部构造带奥陶系岩相、成岩作用带与储层成因[J]. 石油与天然气地质, 2014, 35(6): 870-882. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201406016.htm

    QIAN Yixiong, YU Tengxiao, ZHOU Lingfang, et al. Lithofacies, diagenesis zone and reservoir origin of the Ordovician in eastern tectonic belt of the Maigaiti slope[J]. Oil & Gas Geology, 2014, 35(6): 870-882. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201406016.htm
    [2]
    牛君, 黄文辉, 蒋文龙, 等. 玉北地区奥陶系碳酸盐岩风化壳岩溶储层特征及其主控因素[J]. 东北石油大学学报, 2016, 40(1): 1-13. doi: 10.3969/j.issn.2095-4107.2016.01.001

    NIU Jun, HUANG Wenhui, JIANG Wenlong, et al. Reservoir characterization and controlling factors of Ordovician weathering crust reservoir in Yubei area, Tarim Basin[J]. Journal of Northeast Petroleum University, 2016, 40(1): 1-13. doi: 10.3969/j.issn.2095-4107.2016.01.001
    [3]
    刘忠宝, 高山林, 岳勇, 等. 塔里木盆地麦盖提斜坡奥陶系储层成因与分布[J]. 石油学报, 2014, 35(4): 654-663. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201404005.htm

    LIU Zhongbao, GAO Shanlin, YUE Yong, et al. Formation and distribution of the Ordovician reservoir in Maigaiti slope, Tarim Basin[J]. Acta Petrolei Sinica, 2014, 35(4): 654-663. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201404005.htm
    [4]
    张旭光. 玉北地区碳酸盐岩储层地震响应特征研究[J]. 石油物探, 2012, 51(5): 493-501. doi: 10.3969/j.issn.1000-1441.2012.05.011

    ZHANG Xuguang. Study on seismic response characteristics of carbonate reservoir in Yubei area[J]. Geophysical Prospecting for Petroleum, 2012, 51(5): 493-501. doi: 10.3969/j.issn.1000-1441.2012.05.011
    [5]
    黄太柱. 塔里木盆地玉北地区断裂系统解析[J]. 石油与天然气地质, 2014, 35(1): 98-106. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201401013.htm

    HUANG Taizhu. Analysis on the fault system of Yubei region, Tarim Basin[J]. Oil & Gas Geology, 2014, 35(1): 98-106. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201401013.htm
    [6]
    陈刚, 汤良杰, 余腾孝, 等. 塔里木盆地玉北地区断裂构造差异变形及其控制因素[J]. 地球科学与环境学报, 2015, 37(3): 42-54. doi: 10.3969/j.issn.1672-6561.2015.03.007

    CHEN Gang, TANG Liangjie, YU Tengxiao, et al. Differential deformation and control mechanism of fault structures in Yubei area of Tarim Basin[J]. Journal of Earth Sciences and Environment, 2015, 37(3): 42-54. doi: 10.3969/j.issn.1672-6561.2015.03.007
    [7]
    李慧莉, 刘士林, 杨圣彬, 等. 塔中—巴麦地区构造沉积演化及其对奥陶系储层的控制[J]. 石油与天然气地质, 2014, 35(6): 883-892. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201406017.htm

    LI Huili, LIU Shilin, YANG Shengbin, et al. Tectonic-sedimentary evolution of Tazhong-Bachu-Maigaiti area and its control on the Ordovician reservoir[J]. Oil & Gas Geology, 2014, 35(6): 883-892. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201406017.htm
    [8]
    马海陇, 王震, 邓光校, 等. 塔里木盆地和田河东地区断裂特征及其油气地质意义[J]. 断块油气田, 2021, 28(3): 329-334. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202103009.htm

    MA Hailong, WANG Zhen, DENG Guangxiao, et al. Fault features in eastern Hetianhe area, Tarim Basin and its petroleum geological significance[J]. Fault-Block Oil and Gas Field, 2021, 28(3): 329-334. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202103009.htm
    [9]
    于浩雨, 于明德, 李洲, 等. 洛伊凹陷西南部边界大断裂发育特征及其对油气成藏的控制作用[J]. 油气地质与采收率, 2020, 27(5): 13-24. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS202005003.htm

    YU Haoyu, YU Mingde, LI Zhou, et al. Development characteristics of large fault in southwest boundary of Luoyi Sag and its controlling effect on hydrocarbon accumulation[J]. Petroleum Geology and Recovery Efficiency, 2020, 27(5): 13-24. https://www.cnki.com.cn/Article/CJFDTOTAL-YQCS202005003.htm
    [10]
    于爱暄, 王有功, 刘世瑞, 等. 真武—汉留断裂带分段生长及其油气意义[J]. 特种油气藏, 2020, 27(3): 27-33. doi: 10.3969/j.issn.1006-6535.2020.03.005

    YU Aixuan, WANG Yougong, LIU Shirui, et al. Segmented growth of Zhenwu-Hanliu fault zone and its hydrocarbon significance[J]. Specail Oil & Gas Reservoirs, 2020, 27(3): 27-33. doi: 10.3969/j.issn.1006-6535.2020.03.005
    [11]
    吴梅莲, 刘永福, 彭鹏, 等. 轮南古潜山走滑断裂特征及其对油气成藏的影响[J]. 断块油气田, 2021, 28(4): 456-462. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202104006.htm

    WU Meilian, LIU Yongfu, PENG Peng, et al. Characteristics of strike-slip faults in Lunnan buried hill and its influence on hydrocarbon accumulation[J]. Fault-Block Oil and Gas Field, 2021, 28(4): 456-462. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202104006.htm
    [12]
    汤好书, 陈衍景, 武广, 等. 辽东辽河群大石桥组碳酸盐岩稀土元素地球化学及其对Lomagundi事件的指示[J]. 岩石学报, 2009, 25(11): 3075-3093. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200911036.htm

    TANG Haoshu, CHEN Yanjing, WU Guang, et al. Rare earth element geochemistry of carbonates of Dashiqiao Formation, Liaohe Group, eastern Liaoning province: implications for Lomagundi Event[J]. Acta Petrologica Sinica, 2009, 25(11): 3075-3093. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200911036.htm
    [13]
    崔军文. 南阿尔金断裂的韧性剪切作用时代及其构造意义[J]. 岩石学报, 2011, 27(11): 3422-3434. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201111021.htm

    CUI Junwen. Ductile shearing age of the South Altun fault and its tectonic implications[J]. Acta Petrologica Sinica, 2011, 27(11): 3422-3434. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201111021.htm
    [14]
    黄思静, 卿海若, 胡作维, 等. 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[J]. 地球科学(中国地质大学学报), 2008, 33(1): 26-34. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200801007.htm

    HUANG Sijing, QING Hairuo, HU Zuowei, et al. Cathodoluminescence and diagenesis of the carbonate rocks in Feixianguan Formation of Triassic, eastern Sichuan Basin of China[J]. Earth Science(Journal of China University of Geosciences), 2008, 33(1): 26-34. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200801007.htm
    [15]
    MCLENNAN S M. Relationships between the trace element composition of sedimentary rocks and upper continental crust[J]. Geochemistry, Geophysics, Geosystems, 2001, 2(4): 2000GC000109.
    [16]
    MCARTHUR J M, HOWARTH R J, BAILEY T R. Strontium isotope stratigraphy: LOWESS version 3: best fit to the marine Sr-isotope curve for 0-509 Ma and accompanying look-up table for deriving numerical age[J]. The Journal of Geology, 2001, 109(2): 155-170.
    [17]
    ELDERFIELD H, UPSTILL-GODDARD R, SHOLKOVITZ E R. The rare earth elements in rivers, estuaries, and coastal seas and their significance to the composition of ocean waters[J]. Geochimica et Cosmochimica Acta, 1990, 54(4): 971-991.
    [18]
    BANNER J L, HANSON G N, MEYERS W J. Rare earth element and Nd isotopic variations in regionally extensive dolomites from the Burlington-Keokuk formation (Mississippian): implications for REE mobility during carbonate diagenesis[J]. Journal of Sedimentary Research, 1988, 58(3): 415-432.
    [19]
    QING Hairuo, MOUNTJOY E W. Rare earth element geochemistry of dolomites in the Middle Devonian Presqu'ile barrier, Western Canada Sedimentary Basin: implications for fluid-rock ratios during dolomitization[J]. Sedimentology, 1994, 41(4): 787-804.
    [20]
    PALMER M R. Rare earth elements in foraminifera tests[J]. Earth and Planetary Science Letters, 1985, 73(2/4): 285-298.
    [21]
    MICHARD A, ALBARÈDE F. The REE content of some hydrothermal fluids[J]. Chemical Geology, 1986, 55(1/2): 51-60.
    [22]
    OLIVAREZ A M, OWEN R M. The europium anomaly of seawater: implications for fluvial versus hydrothermal REE inputs to the oceans[J]. Chemical Geology, 1991, 92(4): 317-328.
    [23]
    ALEXANDER B W, BAU M, ANDERSSON P, et al. Continentally-derived solutes in shallow Archean seawater: rare earth element and Nd isotope evidence in iron formation from the 2.9 Ga Pongola Supergroup, South Africa[J]. Geochimica et Cosmochimica Acta, 2008, 72(2): 378-394.
    [24]
    DEBRUYNE D, HULSBOSCH N, MUCHEZ P. Unraveling rare earth element signatures in hydrothermal carbonate minerals using a source-sink system[J]. Ore Geology Reviews, 2016, 72: 232-252.
    [25]
    ROBBINS L J, LALONDE S V, PLANAVSKY N J, et al. Trace elements at the intersection of marine biological and geochemical evolution[J]. Earth-Science Reviews, 2016, 163: 323-348.
    [26]
    BAU M, BALAN S, SCHMIDT K, et al. Rare earth elements in mussel shells of the Mytilidae family as tracers for hidden and fossil high-temperature hydrothermal systems[J]. Earth and Planetary Science Letters, 2010, 299(3/4): 310-316.
    [27]
    王宇航, 朱园园, 黄建东, 等. 海相碳酸盐岩稀土元素在古环境研究中的应用[J]. 地球科学进展, 2018, 33(9): 922-932. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201809006.htm

    WANG Yuhang, ZHU Yuanyuan, HUANG Jiandong, et al. Application of rare earth elements of the marine carbonate rocks in paleoenvironmental researches[J]. Advances in Earth Science, 2018, 33(9): 922-932. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201809006.htm
    [28]
    BAU M, KOSCHINSKY A, DULSKI P, et al. Comparison of the partitioning behaviours of yttrium, rare earth elements, and titanium between hydrogenetic marine ferromanganese crusts and seawater[J]. Geochimica et Cosmochimica Acta, 1996, 60(10): 1709-1725.
    [29]
    SHIELDS G A, WEBB G E. Has the REE composition of seawater changed over geological time?[J]. Chemical Geology, 2004, 204(1/2): 103-107.
    [30]
    ZHANG Jing, NOZAKI Y. Rare earth elements and yttrium in seawater: ICP-MS determinations in the East Caroline, Coral Sea, and South Fiji Basins of the western South Pacific Ocean[J]. Geochimica et Cosmochimica Acta, 1996, 60(23): 4631-4644.
    [31]
    GARCÍA M G, LECOMTE K L, PASQUINI A I, et al. Sources of dissolved REE in mountainous streams draining granitic rocks, Sierras Pampeanas (Córdoba, Argentina)[J]. Geochimica et Cosmochimica Acta, 2007, 71(22): 5355-5368.
    [32]
    BAU M, DULSKI P. Comparing yttrium and rare earths in hydrothermal fluids from the Mid-Atlantic Ridge: implications for Y and REE behaviour during near-vent mixing and for the Y/Ho ratio of Proterozoic seawater[J]. Chemical Geology, 1999, 155(1/2): 77-90.
    [33]
    WHEAT C G, MOTTL M J, RUDNICKI M. Trace element and REE composition of a low-temperature ridge-flank hydrothermal spring[J]. Geochimica et Cosmochimica Acta, 2002, 66(21): 3693-3705.
    [34]
    DOUVILLE E, BIENVENU P, CHARLOU J L, et al. Yttrium and rare earth elements in fluids from various deep-sea hydrothermal systems[J]. Geochimica et Cosmochimica Acta, 1999, 63(5): 627-643.
    [35]
    SMEDLEY P L. The geochemistry of rare earth elements in groundwater from the Carnmenellis area, southwest England[J]. Geochi-mica et Cosmochimica Acta, 1991, 55(10): 2767-2779.
    [36]
    胡文瑄, 陈琪, 王小林, 等. 白云岩储层形成演化过程中不同流体作用的稀土元素判别模式[J]. 石油与天然气地质, 2010, 31(6): 810-818. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201006017.htm

    HU Wenxuan, CHEN Qi, WANG Xiaolin, et al. REE models for the discrimination of fluids in the formation and evolution of dolomite reservoirs[J]. Oil & Gas Geology, 2010, 31(6): 810-818. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201006017.htm
    [37]
    MCARTHUR J M, BURNETT J, HANCOCK J M. Strontium isotopes at K/T boundary[J]. Nature, 1992, 355(6355): 28.
    [38]
    PALMER M R, ELDERFIELD H. Sr isotope composition of sea water over the past 75 Myr[J]. Nature, 1985, 314(6011): 526-528.
    [39]
    PALMER M R, EDMOND J M. The strontium isotope budget of the modern ocean[J]. Earth and Planetary Science Letters, 1989, 92(1): 11-26.
    [40]
    MOORE C H, CHOWDHURY A, CHAN L. Upper Jurassic Smackover platform dolomitization, northwestern gulf of Mexico: a tale of two waters[M]//SHUKLA V, BAKER P A. Sedimentology and Geochemistry of Dolostones. Tulsa: SEPM, 1988: 175-189.
    [41]
    游声刚. 塔里木盆地玉北地区古构造演化对奥陶系岩溶储层的控制作用[D]. 北京: 中国地质大学(北京), 2013.

    YOU Shenggang. Controlling effect of paleotectonic evolution on Ordovician karst reservoir in Yubei area of Tarim Basin[D]. Beijing: China University of Geosciences(Beijing), 2013.
    [42]
    陈刚, 汤良杰, 余腾孝, 等. 塔里木盆地玉北冲断带分期活动特征及其控油气作用[J]. 中国矿业大学学报, 2014, 43(5): 870-879. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGKD201405016.htm

    CHEN Gang, TANG Liangjie, YU Tengxiao, et al. Poly-phase fault activities and the control on hydrocarbon accumulation of Yubei thrust belt, Tarim Basin[J]. Journal of China University of Mining & Technology, 2014, 43(5): 870-879. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGKD201405016.htm
    [43]
    丁文龙, 漆立新, 云露, 等. 塔里木盆地巴楚—麦盖提地区古构造演化及其对奥陶系储层发育的控制作用[J]. 岩石学报, 2012, 28(8): 2542-2556. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201208021.htm

    DING Wenlong, QI Lixin, YUN Lu, et al. The tectonic evolution and its controlling effects on the development of ordovician reservoir in Bachu-Markit Tarim Basin[J]. Acta Petrologica Sinica, 2012, 28(8): 2542-2556. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201208021.htm
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    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

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(9)  / Tables(1)

    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (326) PDF downloads(54) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return