留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

松辽盆地大庆长垣南缘四方台组砂岩型铀矿碳氧同位素特征及铀成矿意义

蔡宁宁 邹妞妞 付勇 魏帅超 李建国 汤超 魏佳林

蔡宁宁, 邹妞妞, 付勇, 魏帅超, 李建国, 汤超, 魏佳林. 松辽盆地大庆长垣南缘四方台组砂岩型铀矿碳氧同位素特征及铀成矿意义[J]. 地质科技通报, 2021, 40(3): 140-150. doi: 10.19509/j.cnki.dzkq.2021.0307
引用本文: 蔡宁宁, 邹妞妞, 付勇, 魏帅超, 李建国, 汤超, 魏佳林. 松辽盆地大庆长垣南缘四方台组砂岩型铀矿碳氧同位素特征及铀成矿意义[J]. 地质科技通报, 2021, 40(3): 140-150. doi: 10.19509/j.cnki.dzkq.2021.0307
Cai Ningning, Zou Niuniu, Fu Yong, Wei Shuaichao, Li Jianguo, Tang Chao, Wei Jialin. Carbon and oxygen isotopic characteristics and uranium mineralization significance of the sandstone-type uranium deposit in the Sifangtai Formation at the southern margin of Daqing placanticline in Songliao Basin[J]. Bulletin of Geological Science and Technology, 2021, 40(3): 140-150. doi: 10.19509/j.cnki.dzkq.2021.0307
Citation: Cai Ningning, Zou Niuniu, Fu Yong, Wei Shuaichao, Li Jianguo, Tang Chao, Wei Jialin. Carbon and oxygen isotopic characteristics and uranium mineralization significance of the sandstone-type uranium deposit in the Sifangtai Formation at the southern margin of Daqing placanticline in Songliao Basin[J]. Bulletin of Geological Science and Technology, 2021, 40(3): 140-150. doi: 10.19509/j.cnki.dzkq.2021.0307

松辽盆地大庆长垣南缘四方台组砂岩型铀矿碳氧同位素特征及铀成矿意义

doi: 10.19509/j.cnki.dzkq.2021.0307
基金项目: 

国家重点研发项目 2019YFC1805300

国家自然科学基金 41802174

贵州省科技厅计划 黔科合基础〔2019〕1119

贵州大学2017年度学术新苗培养及创新探索专项 黔科合平台人才〔2017〕7285

贵州大学引进人才科研项目 贵大人基合字〔2016〕82号

贵州省人才基地项目 RCJD2018-21

详细信息
    作者简介:

    蔡宁宁(1996-), 男, 正在攻读矿产普查与勘探专业硕士学位, 主要从事铀矿方面的研究。E-mail: cainn0617@163.com

    通讯作者:

    邹妞妞(1989-), 女, 副教授, 主要从事沉积学、沉积矿产方面的研究工作。E-mail: niuniu9728@126.com

  • 中图分类号: P597+.2

Carbon and oxygen isotopic characteristics and uranium mineralization significance of the sandstone-type uranium deposit in the Sifangtai Formation at the southern margin of Daqing placanticline in Songliao Basin

  • 摘要: 为进一步探讨松辽盆地大庆长垣南缘四方台组砂岩型铀矿的成岩环境、铀沉淀机制及成矿机理,通过钻井岩心观察,岩石薄片,含铀砂岩碳酸盐胶结物碳、氧同位素分析,对研究区砂岩岩石类型、碳酸盐胶结物类型、成岩阶段以及碳、氧同位素特征进行了系统研究。结果表明:含铀砂岩岩石类型为长石岩屑砂岩、岩屑长石砂岩,碳酸盐胶结物可分为3个期次,以第一和第二期次为主,胶结物包括方解石、铁方解石,见极少量含铁白云石。δ13CPDB值为-22.45‰~-13.65‰,平均值为-18.33‰,δ18OPDB值为-17.56‰~-9.46‰,平均值为-13.52‰,揭示有一定有机质参与;古盐度Z值介于75.98~90.97之间,为淡水沉积;古温度介于67.31~94.92℃之间,结合以上岩石特征、胶结物类型及成岩作用判定成岩环境处于早成岩—中成岩阶段A期。综合分析认为:早成岩阶段砂岩的压实、胶结作用使含铀砂岩孔隙度减小,抑制含氧富铀流体运移;随着成岩作用进行,埋藏深度增加,有机质成熟度升高发生热脱羧基作用,与压实作用产生的吸附水形成酸性溶液对长石、碳酸盐胶结物等进行溶蚀形成次生孔隙,增大砂岩孔隙度,促进含氧富铀流体下渗运移,下伏油气由断裂向上逸散,为地层提供还原剂,使铀在四方台组底部大规模沉淀和富集。

     

  • 图 1  松辽盆地区域地质图及研究区钻孔分布图

    Figure 1.  Regional geological map and borehole distribution map of Songliao Basin

    图 2  松辽盆地研究区钻孔(5D901-1)地层综合柱状图

    Figure 2.  Comprehensive column chart of borehole(5D901-1) formation in Songliao Basin

    图 3  研究区四方台组显微照片

    a.灰色细砂岩,颗粒呈点接触、点-线接触,ZKDX00-02钻孔,样品DX2-16,318.4 m,单偏光;b.浅灰色细砂岩,第一期碳酸盐胶结物类型为泥晶方解石,ZKDX00-01钻孔,样品DX-13,418 m,单偏光;c.浅灰色细砂岩,碳酸盐胶结物类型为方解石,ZKDX00-01钻孔,样品DX-30,410 m,正交偏光;d.灰色细砂岩,第二期碳酸盐胶结物为铁方解石(紫红色),ZKDX00-02钻孔,样品DX2-16,318.4 m,正交偏光;e.浅灰绿色细砂岩,碎屑颗粒受挤压力作用产生破裂,ZKDX00-01钻孔,样品DX-39,406.8 m,单片光;f.灰色细砂岩,第三期碳酸盐胶结物极少量含铁白云石(亮蓝色)充填于油气充填剩余粒间孔隙,5D1-17, 384.2 m,单偏光;g.灰色中砂岩,长石颗粒表面不干净,形成溶蚀孔隙,长石岩屑颗粒形状部分被溶蚀,5D901-1钻孔,样品5D1-5,324 m,单偏光;h.灰色细砂岩,石英加大边,ZKDX00-01钻孔,样品DX2-16,318.4 m,正交偏光;i.灰色细砂岩,粒间草莓状黄铁矿,5D901-1钻孔,样品5D1-15,319.2 m,反射光

    Figure 3.  Micrograph of Sifangtai formation in the study area

    图 4  研究区四方台组含铀砂岩碳酸盐胶结物碳氧同位素成因图解(底图据考文献[22])

    Figure 4.  Diagram of carbon and oxygen isotope genesis of carbonate cement of uranium bearing sandstone in Sifangtai formation

    图 5  研究区四方台组含铀砂岩方解石胶结物18OSMOW-δ13CPDB图解(底图据文献[26])

    Figure 5.  Diagram of 18OSMOW-δ13CPDB calcite cement of uranium-bearing sandstone in Sifangtai Formation

    图 6  研究区四方台组含铀砂岩碳酸盐胶结物沉积温度分布图

    Figure 6.  Deposition temperature distribution of carbonate cements of uranium-bearing sandstone in the Sifangtai Formation in the study area

    图 7  研究区四方台组含铀砂岩部分钻孔柱状图

    Figure 7.  Borehole histogram of part of uranium-bearing sandstone of Sifangtai Formation in the study area

    表  1  研究区四方台组含铀砂岩碳酸盐胶结物碳氧同位素及U质量分数测试结果

    Table  1.   Testing results of carbon and oxygen isotopes and U content of carbonate cement in Sifangtai Formation

    钻孔 样号 岩性 深度/m δ13CPDB/‰ δ18OPDB/‰ δ18OSMOW/‰ w(U)/(μg·g-1) T/℃ Z
    ZKDX00-01 DX-67 浅灰绿色细砂岩 379.90 -19.96 -11.23 19.34 2.30 78.70 80.82
    DX-62 浅灰色粉砂岩 382.00 -17.73 -14.72 15.75 56.02 103.03 83.66
    DX-47 灰绿色粉砂质泥岩 400.00 -17.81 -14.27 16.21 3.00 99.75 83.72
    DX-43 浅灰绿色细砂岩 404.40 -17.56 -14.93 15.53 4.64 104.57 83.91
    DX-39 浅灰绿色细砂岩 406.78 -17.87 -14.20 16.28 8.02 99.28 83.63
    DX-30 浅灰色细砂岩 410.00 -16.90 -16.72 13.69 280.98 118.05 84.36
    DX-26 浅灰色细砂岩 411.95 -13.65 -16.81 13.59 214.95 118.80 90.97
    DX-22 浅灰绿色细砂岩 413.85 -18.13 -11.47 19.09 43.61 80.31 84.45
    DX-20 浅灰色细砂岩 413.90 -18.17 -11.14 19.43 11.03 78.13 84.55
    DX-13 浅灰色细砂岩 418.00 -16.11 -15.37 15.08 3.19 107.80 86.65
    DX-11 浅灰色细砂岩 419.30 -15.25 -15.82 14.62 2.52 111.18 88.19
    ZKDX00-02 ZKDX00-2-36 灰绿色细砂岩 290.20 -17.36 -14.64 15.83 3.17 102.42 84.46
    ZKDX00-2-34 灰绿色中砂岩 291.43 -20.54 -12.23 18.31 1.81 85.44 79.15
    ZKDX00-2-33 灰绿色细砂岩 295.00 -17.88 -12.36 18.18 2.12 86.31 84.52
    ZKDX00-2-20 棕色细砂岩 315.00 -20.24 -12.97 17.55 2.78 90.54 79.39
    ZKDX00-2-16 灰色细砂岩 318.40 -21.83 -11.91 18.65 18.99 83.23 76.66
    ZKDX00-2-15 灰色细砂岩 319.10 -22.45 -10.72 19.87 79.12 75.34 75.98
    ZKDX00-2-10 棕色泥岩 324.00 -19.03 -12.27 18.27 1.44 85.71 82.22
    5D901-01 5D1-52 褐红色泥岩 349.50 -16.83 -16.05 14.37 2.92 112.98 84.84
    5D1-45 灰色粉砂岩 354.40 -15.40 -16.24 14.18 81.43 114.43 87.68
    5D1-30 浅灰褐色泥岩 374.00 -15.30 -15.00 15.46 3.26 105.10 88.49
    5D1-27 灰色细砂岩 378.43 -15.63 -15.15 15.31 2.81 106.18 87.75
    5D1-23 灰色细砂岩 381.43 -18.21 -9.46 21.16 3.85 67.31 85.29
    5D1-19 灰色细砂岩 383.00 -19.35 -17.56 12.82 257.16 124.65 78.94
    5D1-18 灰色细砂岩 383.90 -21.00 -9.95 20.67 286.27 70.35 79.33
    5D1-17 灰色细砂岩 384.20 -16.63 -14.54 15.93 10.27 101.71 86.00
    5D1-16 灰色细砂岩 384.90 -20.21 -15.70 14.74 316.10 110.31 78.08
    5D1-15 灰色细砂岩 385.20 -20.34 -11.71 18.84 334.27 81.93 79.82
    5D1-12 灰色细砂岩 386.50 -22.08 -10.05 20.56 463.65 70.99 77.07
    5D1-11 灰色细砂岩 387.00 -21.20 -10.31 20.30 401.61 72.65 78.75
    5D1-10 灰色细砂岩 387.50 -16.87 -15.11 15.35 494.36 105.80 85.22
    5D1-8 灰色含砾细砂岩 389.60 -19.46 -12.24 18.30 385.06 85.47 81.35
    5D1-5 灰色中砂岩 392.01 -18.05 -13.42 17.09 8.77 93.69 83.65
    注:氧同位素SOMW标准与PDB标准换算关系为:δ18OSMOW=1.030 91;δ18OPDB+30.91[24]
    下载: 导出CSV
  • [1] 陈戴生, 李胜祥, 蔡煜琦. 我国中生代盆地砂岩型铀矿研究现状及发展方向的探讨[J]. 沉积学报, 2003, 21(1): 113-117. doi: 10.3969/j.issn.1000-0550.2003.01.017

    Chen D S, Li S X, Cai Y Q. A Discussion on research situation and development direction of sandstone-type uranium deposits in the meso-cenozoic basin of China[J]. Acta Sedimentologica Sinica, 2003, 21(1): 113-117(in Chinese with English abstract). doi: 10.3969/j.issn.1000-0550.2003.01.017
    [2] 张金带, 李友良, 简晓飞. 我国铀资源勘查状况及发展前景[J]. 中国工程科学, 2008, 10(1): 54-59. doi: 10.3969/j.issn.1009-1742.2008.01.009

    Zhang J D, Li Y L, Jian X F. Situation and development prospect of uranium resources exploration in China[J]. Engineering Science China, 2008, 10(1): 54-59(in Chinese with English abstract). doi: 10.3969/j.issn.1009-1742.2008.01.009
    [3] 刘池洋, 赵红格, 谭成仟, 等. 多种能源矿产赋存与盆地成藏(矿)系统[J]. 石油与天然气地质, 2006, 27(2): 131-142. doi: 10.3321/j.issn:0253-9985.2006.02.001

    Liu C Y, Zhao H G, Tan C Q, et al. Occurrences of multiple energy mineral deposits and mineralization/reservoiring system in the basin[J]. Oil & Gas Geology, 2006, 27(2): 131-142(in Chinese with English abstract). doi: 10.3321/j.issn:0253-9985.2006.02.001
    [4] 杨伟利, 王毅, 王传刚, 等. 鄂尔多斯盆地多种能源矿产分布特征与协同勘探[J]. 地质学报, 2010, 84(4): 579-586. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201004013.htm

    Yang W L, Wang Y, Wang C G, et al. Distribution and co-exploration of multiple energy minerals in Ordos Basin[J]. Acta Geologica Sinica, 2010, 84(4): 579-586(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201004013.htm
    [5] 朱西养, 彭新建, 汪云亮, 等. 新疆十红滩层间氧化带型砂岩铀矿同位素地球化学研究[J]. 矿床地质, 2004, 23(4): 443-451. doi: 10.3969/j.issn.0258-7106.2004.04.004

    Zhu X Y, Peng X J, Wang Y L, et al. Isotope geochemistry of Shihongtan interlayer oxidized zone type sandstone uranium deposit[J]. Mineral Deposits, 2004, 23(4): 443-451(in Chinese with English abstract). doi: 10.3969/j.issn.0258-7106.2004.04.004
    [6] 刘武生, 赵兴齐, 史清平, 等. 中国北方砂岩型铀矿成矿作用与油气关系研究[J]. 中国地质, 2017, 44(2): 279-287. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201702006.htm

    Liu W S, Zhao X Q, Shi Q P, et al. Research on relationship of oil-gas and sandstone-type uranium mineralization of northern China[J]. Geology of China, 2017, 44(2): 279-287(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201702006.htm
    [7] 佘新民, 赵军龙, 崔建华, 等. 松辽盆地西南部白兴吐地段铀成矿地质条件及找矿方向分析[J]. 铀矿地质, 2007, 23(4): 201-206. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200704001.htm

    She X M, Zhao J L, Cui J H, et al. Analysis on geology condition of uranium mineralization and the exploration orientation for Baixingtu district southwestern Songliao Basin[J]. Uranium Geology, 2007, 23(4): 201-206(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200704001.htm
    [8] 徐喆, 吴仁贵, 余达淦, 等. 松辽盆地砂岩型铀矿床的热液作用特征: 以宝龙山地段砂岩铀矿为例[J]. 东华理工大学学报: 自然科学版, 2011, 34(3): 201-208. https://www.cnki.com.cn/Article/CJFDTOTAL-HDDZ201103003.htm

    Xu Z, Wu R G, Yu D G, et al. Features of hydrothermal alteration of sandstone-type uranium in Songliao Basin: A case of study in sandstone-type uranium deposit of Baolongshan Section[J]. Journal of East China Institute of Technology (Natural Science Edition), 2011, 34(3): 201-208(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-HDDZ201103003.htm
    [9] 陈路路, 汤超, 李建国, 等. 松辽盆地大庆长垣南端四方台组含铀砂岩岩石学特征及地质意义[J]. 地质调查与研究, 2018, 41(1): 33-39. doi: 10.3969/j.issn.1672-4135.2018.01.005

    Chen L L, Tang C, Li J G, et al. Petrology characteristics of the uranium-bearing layer of Sifangtai Formation in Daqing placanticline of Songliao Basin and their geological implications[J]. Geological Survey and Research, 2018, 41(1): 33-39(in Chinese with English abstract). doi: 10.3969/j.issn.1672-4135.2018.01.005
    [10] 刘招君, 杨虎林, 董清水, 等. 中国油页[M]. 北京: 石油工业出版社, 2009.

    Liu Z J, Yang H L, Dong Q S, et al. Oil pages in China[M]. Beijing: Petroleum Industry Press, 2009(in Chinese with English abstract).
    [11] 李建国, 金若时, 张博, 等. 松辽盆地西南部上白垩统姚家组原生黏土矿物组合特征及其找铀意义[J]. 地球学报, 2018, 39(3): 295-305. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201803004.htm

    Li J G, Jin R S, Zhang B, et al. Characteristics of primary clay minerals in the upper cretaceous Yaojia Formation of southwest Songliao Basin and their significance[J]. Acta Geoscientia Sinica, 2018, 39(3): 295-305(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201803004.htm
    [12] 汤超, 金若时, 谷社峰, 等. 松辽盆地北部四方台组工业铀矿体的发现及其意义[J]. 地质调查与研究, 2018, 41(1): 1-8. doi: 10.3969/j.issn.1672-4135.2018.01.001

    Tang C, Jin R S, Gu S F, et al. Discovery and significance of industrial uranium ore in Sifangtai Formation, north Songliao Basin[J]. Geological Survey and Research, 2018, 41(1): 1-8(in Chinese with English abstract). doi: 10.3969/j.issn.1672-4135.2018.01.001
    [13] 王琪, 郝乐伟, 陈国俊, 等. 白云凹陷珠海组砂岩中碳酸盐胶结物的形成机理[J]. 石油学报, 2010, 31(4): 553-558. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201004005.htm

    Wang Q, Hao L W, Chen G J, et al. Forming mechanism of carbonate cements in siliciclastic sandstone of Zhuhai Formation in Baiyun Sag[J]. Acta Petrolei Sinica, 2010, 31(4): 553-558(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201004005.htm
    [14] 邓硕, 刘招君, 孙平昌. 松辽盆地东南隆起区上白垩统嫩江组泥页岩段地球化学特征与物源分析[J]. 世界地质, 2016, 35(1): 108-122. doi: 10.3969/j.issn.1004-5589.2016.01.011

    Deng S, Liu Z J, Sun P C. Geochemical characteristics and implications for provenance of shale from Upper Cretaceous Nenjiang Formation of southeastern uplifted area in Songliao Basin[J]. Global Geology, 2016, 35(1): 108-122(in Chinese with English abstract). doi: 10.3969/j.issn.1004-5589.2016.01.011
    [15] 魏帅超, 邹妞妞, 付勇, 等. 松辽盆地××地区四方台组富铀地层的微量元素地球化学特征[J]. 矿物学报, 2019, 39(6): 697-708. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB201906010.htm

    Wei S C, Zou N N, Fu Y, et al. Geochemical characteristics of trace elements in a uranium-rich bed of Sifangtai Formation in the Songliao Basin[J]. Acta Mineralogica Sinica, 2019, 39(6): 697-708(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB201906010.htm
    [16] 张兴洲, 杨宝俊, 吴福元, 等. 中国兴蒙-吉黑地区岩石圈结构基本特征[J]. 中国地质, 2006, 33(4): 816-823. doi: 10.3969/j.issn.1000-3657.2006.04.011

    Zhang X Z, Yang B J, Wu F Y, et al. The lithosphere structure in the Hingmong-Jihei (Hinggan-Mongolia-Jilin-Heilongjiang) region, northeastern China[J]. Geology of China, 2006, 33(4): 816-823(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2006.04.011
    [17] 刘招君, 王东坡, 刘立, 等. 松辽盆地白垩纪沉积特征[J]. 地质学报, 1992, 66(4): 327-338. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199204004.htm

    Liu Z J, Wang D P, Liu L, et al. Sedimentary characteristics of the cretaceous in the Songliao Basin[J]. Acta Geologica Sinica, 1992, 66(4): 327-338(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199204004.htm
    [18] 舒良树, 慕玉福, 王伯长. 松辽盆地含油气地层及其构造特征[J]. 地层学杂志, 2003, 27(4): 340-349. doi: 10.3969/j.issn.0253-4959.2003.04.014

    Shu L S, Mu Y F, Wang B C. The oil-gas-bearing strata and the structural features in the Songliao Basin, Ne China[J]. Journal of Stratigraphy, 2003, 27(4): 340-349(in Chinese with English abstract). doi: 10.3969/j.issn.0253-4959.2003.04.014
    [19] 魏佳林, 汤超, 徐增连, 等. 大庆长垣南部四方台组砂岩型铀矿化特征研究[J]. 地质调查与研究, 2018, 41(1): 9-17. doi: 10.3969/j.issn.1672-4135.2018.01.002

    Wei J L, Tang C, Xu Z L, et al. Research on sandstone-hosted uranium mineralization of the Sifangtai Formation in southern Daqing placanticline[J]. Geological Survey and Research, 2018, 41(1): 9-17(in Chinese with English abstract). doi: 10.3969/j.issn.1672-4135.2018.01.002
    [20] 程日辉, 王国栋, 王璞珺, 等. 松科1井北孔四方台组-明水组沉积微相及其沉积环境演化[J]. 地学前缘, 2009, 16(6): 85-95. doi: 10.3321/j.issn:1005-2321.2009.06.009

    Cheng R H, Wang G D, Wang P J, et al. Uppermost Cretaceous sediments: Sedimentary microfacies and sedimentary environment evolution of Sifangtai Formation and Mingshui Formation in SK-Ⅰ(n)[J]. Earth Science Frontiers, 2009, 16(6): 85-95(in Chinese with English abstract). doi: 10.3321/j.issn:1005-2321.2009.06.009
    [21] 郑永飞, 陈江峰. 稳定同位素地球化学特征[M]. 北京: 科学出版社, 2000.

    Zheng Y F, Chen J F. Geochemical characteristics of stable isotopes[M]. Beijing: Science Press, 2000(in Chinese with English abstract).
    [22] Mack G H, Cole D R, Giordano T H, et al. Paleoclimatic controls on stable oxygen and carbon isotopes in caliche of the Abo Formation (Permian), south-central New Mexico, U.S.A. [J]. Journal of Sedimentary Research, 1991, 61(4): 458-472.
    [23] 冯乔, 张小莉, 王云鹏, 等. 鄂尔多斯盆地北部上古生界油气运聚特征及其铀成矿意义[J]. 地质学报, 2006, 80(5): 748-752. doi: 10.3321/j.issn:0001-5717.2006.05.016

    Feng Q, Zhang X L, Wang Y P, et al. Characteristics of migration and accumulation of hydrocarbon and its deposit-forming signification in Upper Paleozoic in North Ordos Basin[J]. Acta Geologica Sinica, 2006, 80(5): 748-752(in Chinese with English abstract). doi: 10.3321/j.issn:0001-5717.2006.05.016
    [24] Coplen T B, Kendall C, Hopple J. Comparison of stable isotope reference material samples[J]. Nature, 1983, 302: 236-238. doi: 10.1038/302236a0
    [25] 王大锐. 油气稳定同位素地球化学[M]. 北京: 地质出版社, 2000.

    Wang D R. Stable isotope geochemistry of oil and gas[M]. Beijing: Geological Press, 2000(in Chinese with English abstract).
    [26] 刘建明, 刘家军, 顾雪祥. 沉积盆地中的流体活动及其成矿作用[J]. 岩石矿物学杂志, 1997, 14(4): 341-351. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW704.006.htm

    Liu J M, Liu J J, Gu X X. Basin fluids and their related ore deposits[J]. Acta Petrological et Mineralogica, 1997, 14(4): 341-351(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW704.006.htm
    [27] 吴柏林, 魏安军, 刘池洋, 等. 鄂尔多斯盆地北部延安组白色砂岩形成的稳定同位素示踪及其地质意义[J]. 地学前缘, 2015, 22(3): 205-214. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201503020.htm

    Wu B L, Wei A J, Liu C Y, et al. Stable isotope tracing on the formation of white sandstone in Yan'an Group, northern Ordos Basin, and its geological significance[J]. Earth Science Frontiers, 2015, 22(3): 205-214(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201503020.htm
    [28] 罗霞, 孙粉锦, 邵明礼, 等. 松辽盆地深层煤型气与气源岩地球化学特征[J]. 石油勘探与开发, 2009, 36(3): 339-346. doi: 10.3321/j.issn:1000-0747.2009.03.009

    Luo X, Sun F J, Shao M L, et al. Geochemistry of deep coal-type gas and gas source rocks in Songliao Basin[J]. Petroleum Exploration and Development, 2009, 36(3): 339-346(in Chinese with English abstract). doi: 10.3321/j.issn:1000-0747.2009.03.009
    [29] 刘阳, 王军礼, 李建国, 等. 松辽盆地北部大庆长垣上白垩统四方台组精细地层划分及其铀成矿意义[J]. 地层学杂志, 2020, 44(2): 181-190. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ202002006.htm

    Liu Y, Wang J L, Li J G, et al. Fine stratigraphic division of the upper cretaceous Sifangtai Formation in the Daqing placanticline, northern SongLiao basin and its significance for uranium mineralization[J]. Journal of Stratigraphy, 2020, 44(2): 181-190(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ202002006.htm
    [30] 付秀丽, 张顺, 梁江平. 松辽盆地北部浅层次生油气藏成藏特征[J]. 天然气工业, 2010, 30(4): 29-34. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201004010.htm

    Fu X L, Zhang S, Liang J P. Characteristics of hydrocarbon accumulation in the shallow secondary reservoirs in the northern Songliao Basin[J]. Natural Gas Industry, 2010, 30(4): 29-34(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201004010.htm
    [31] 程璇, 徐尚, 郝芳, 等. 松辽盆地嫩江组富有机质页岩有机孔隙成因[J]. 地质科技情报, 2019, 38(4): 62-69. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904008.htm

    Cheng X, Xu S, Hao F, et al. Origin of organic pores in the organic-rich shale of Nenjiang Formation, Songliao Basin, China[J]. Geological Science and Technology Information, 2019, 38(4): 62-69(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904008.htm
    [32] 钟延秋. 大庆长垣构造演化特征及对砂岩型铀矿成矿的控制作用[J]. 东华理工大学学: 自然科学版, 2012, 35(4): 315-321. https://www.cnki.com.cn/Article/CJFDTOTAL-HDDZ201204005.htm

    Zhong Y Q. Tectonic evolution and control effect on sandstone-type uranium mineralization in Changqi Placantieline[J]. East China Institute of Technology (Natural Science), 2012, 35(4): 315-321(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-HDDZ201204005.htm
    [33] 夏丹. 松辽盆地构造隆幅影响因素及与油气藏形成关系[J]. 大庆石油地质与开发, 2017, 36(3): 13-17. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201703004.htm

    Xia D. Influencing factors of the tectonic uplifts and their relationships with the petroleum accumulation in Songliao Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2017, 36(3): 13-17(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201703004.htm
    [34] 魏佳林, 汤超, 金若时, 等. 松辽盆地北部龙虎泡地区铁钛氧化物与砂岩型铀矿化关系探讨[J]. 岩石矿物学杂志, 2019, 38(3): 375-389. doi: 10.3969/j.issn.1000-6524.2019.03.007

    Wei J L, Tang C, Jin R S, et al. A study of the relationship between the Fe-Ti oxide and sandstone-hosted uranium mineralization in Longhupao area, northern Songliao Basin[J]. Acta Petrologica et Mineralogica, 2019, 38(3): 375-389(in Chinese with English abstract). doi: 10.3969/j.issn.1000-6524.2019.03.007
    [35] 陈荣坤. 稳定氧碳同位素在碳酸盐岩成岩环境研究中的应用[J]. 沉积学报, 1994, 12(4): 11-21. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB404.001.htm

    Chen R K. Application of stable oxygen and carbon isotope in the research of carbonate diagenetic environment[J]. Acta Sedimentologica Sinica, 1994, 12(4): 11-21(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB404.001.htm
    [36] 张秀莲. 碳酸盐岩中氧、碳稳定同位素与古盐度、古水温的关系[J]. 沉积学报, 1985, 3(4): 17-28. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198504001.htm

    Zhang X L. Relationship between carbon and oxygen stable isotope in carbonate rocks and paleosalinity and paleo-temperature of seawater[J]. Acta Sedimentologica Sinica, 1985, 3(4): 17-28(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198504001.htm
    [37] 毛玲玲, 伊海生, 季长军, 等. 柴达木盆地新生代湖相碳酸盐岩岩石学及碳氧同位素特征[J]. 地质科技情报, 2014, 33(1): 41-48. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201401007.htm

    Mao L L, Yi H S, Ji C J, et al. Petrography and carbon-oxygen isotope characteristics of the cenozoic lacustrine carbonate rocks in Qaidam Basin[J]. Geological Science and Technology Information, 2014, 33(1): 41-48(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201401007.htm
    [38] Sanyal P, Bhattacharya S K, Prasad M. Chemical diagenesis of Siwalik sandstone: Isotopic and mineralogical proxies from Surai Khola section, Nepal[J]. Sediment Geology, 2005, 180(1): 57-74. http://www.sciencedirect.com/science/article/pii/S0037073805002228
    [39] 杨晓勇, 罗贤冬, 凌明星. 鄂尔多斯盆地含铀砂岩碳酸盐胶结物C-O同位素研究及地质意义[J]. 中国科学技术大学学报, 2007, 37(8): 979-985. https://www.cnki.com.cn/Article/CJFDTOTAL-ZKJD200708024.htm

    Yang X Y, Luo X D, Ling M X. C-O stable isotopes of carbonate from cements of U-bearing sandstones in the Ordos Basin and their geological significance[J]. Journal of University of Science and Technology of China, 2007, 37(8): 979-985(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-ZKJD200708024.htm
    [40] 李阳, 张文选, 李树同, 等. 鄂尔多斯盆地长8砂岩储层碳酸盐胶结物特征及其对物性的影响[J]. 地质科技情报, 2018, 37(4): 175-183. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201804024.htm

    Li Y, Zhang W X, Li S T, et al. Characteristics of carbonate cements and their effects on properties in Chang 8 sandstone reservoir, Ordos Basin[J]. Geological Science and Technology Information, 2018, 37(4): 175-183(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201804024.htm
    [41] 曹家鑫, 何方方, 朱蓉, 等. 梨树断陷营城组砂岩方解石胶结物碳、氧同位素特征[J]. 地质科技情报, 2018, 37(3): 75-80. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201803010.htm

    Cao J X, He F F, Zhu R, et al. Features of carbon-oxygen isotopes in calcite cement from Yingcheng Formation sandstone in Sujiatun-Pijia area of Lishu fault depression[J]. Geological Science and Technology Information, 2018, 37(3): 75-80(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201803010.htm
    [42] 汤超, 司马献章, 朱强, 等. 东胜地区直罗组含铀砂岩中方解石的碳氧同位素组成及铀成矿意义[J]. 高校地质学报, 2016, 22(4): 698-706. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201604012.htm

    Tang C, Sima X Z, Zhu Q, et al. Carbon and oxygen isotopic composition and uranium mineralization significance of calcite of Zhiluo Formation uranium-bearing sandstones in dongsheng area[J]. Geological Journal of China Universities, 2016, 22(4): 698-706(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201604012.htm
    [43] Keith M L, Weber J N. Isotopic composition and environmental classification of seleeted limestones and fossils[J]. Geochimica et Cosmochimica Acta, 1964, 28(10/11): 1787-1816.
    [44] Surdam R C, Crossey L J, Hagen E S, et al. Organic-inorganic interactions and sandstone diagenesis[J]. AAPG Bulletin, 1989, 73(1): 1-23.
    [45] 唐鑫萍, 王冠群, 钱茂路, 等. 三水盆地古近系布三段砂岩中碳酸盐胶结物特征及成因[J]. 天然气地球科学, 2019, 30(3): 353-360. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201903006.htm

    Tang X P, Wang G Q, Qian M L, et al. Characteristics and formation of carbonate cements of sandstones in Paleogene 3rd member of Buxin Formation of Sanshui Basin[J]. Natural Gas Geoscience, 2019, 30(3): 353-360(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201903006.htm
    [46] 丁晓琪, 韩玫梅, 张哨楠, 等. 大气淡水在碎屑岩次生孔隙中的作用[J]. 地质评论, 2014, 60(1): 145-158. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201401016.htm

    Ding X Q, Han M M, Zhang S N, et al. Roles of meteoric water on secondary porosity of siliciclastic reservoirss[J]. Geological Review, 2014, 60(1): 145-158(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201401016.htm
    [47] Ketzer J M, Morad S, Amorosi A. Predictive diagenetic claymineral distribution in siliciclastic rocks within a sequence stratigraphic framework[J]. Intermational Associational of Sedimentologists, 2003, 15(3/4): 43-61. doi: 10.1002/9781444304336.ch2
    [48] Urey H C, Lowentstam H A, Epstein S, et al. Measurement of palaeotemperatures and temperatures of the upper Cretaceous of England, Denmark, and the southeastern United States[J]. Geol. Soc. Am. Bull., 1951, 26: 399-416.
    [49] Epstein S, Buchsbaum R, Lowenstam H A, et al. Revised carbonatewater isotopic temperature scale[J]. Bulletin of Geology Society of America, 1953, 64(11): 1351-1326. http://www.zhangqiaokeyan.com/academic-journal-foreign_other_thesis/020414237787.html
    [50] Shackleton N J. Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus Uvigerina: Isotopic changes in the ocean during the last glacial[J]. Collques Internationaux Centre National De La Recherche Scientifique, 1974, 219(302): 203-209.
    [51] 何忧, 荣辉, 黄琨, 等. 伊犁盆地水文地质条件与铀成矿的关系[J]. 地质科技通报, 2020, 39(5): 139-147. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202005017.htm

    He Y, Rong H, Huang K, et al. Relationship between uranium mineralization and hydrologic condition in Yili Basin[J]. Bulletin of Geological Science and Technology, 2020, 39(5): 139-147(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202005017.htm
    [52] 王书宝, 孙钰, 钟建华, 等. 松辽盆地晚白垩世古气候变化对层序发育的影响[J]. 石油地质与工程, 2008, 22(4): 29-32, 10. https://www.cnki.com.cn/Article/CJFDTOTAL-SYHN200804012.htm

    Wang S B, Sun Y, Zhong J H, et al. Effect of palaeoclimate change at the late Cretaceous period on lithologic sequences in Songliao Basin[J]. Petroleum Geology and Engineering, 2008, 22(4): 29-32, 10(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYHN200804012.htm
    [53] 樊爱萍, 柳益群, 杨仁超, 等. 鄂尔多斯盆地东胜地区砂岩型铀矿成岩作用研究[J]. 中国科学: 地球科学, 2007(增刊1): 166-172. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2007S1018.htm

    Fan A P, Liu Y Q, Yang R C, et al. Research on diagenesis of the sandstone-type uranium deposits in Dongsheng area, Ordos Basin[J]. Science China (Series D: Earth Sciences), 2007(S1): 166-172(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2007S1018.htm
    [54] 左智峰, 熊鹰, 何为, 等. 鄂尔多斯盆地中部马五段盐下储层成岩作用与孔隙演化[J]. 地质科技情报, 2019, 38(5): 155-164. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201905016.htm

    Zuo Z F, Xiong Y, He W, et al. Diagenesis and porosity evolution of the subsalt member 5 of Majiagou Formation reservoir in the central Ordos Basin[J]. Geological Science and Technology Information, 2019, 38(5): 155-164(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201905016.htm
    [55] 孙国强, 吕婧文, 赵明君, 等. 柴达木盆地鄂博梁Ⅲ号中新统成岩作用及沉积环境[J]. 沉积学报, 2015, 33(2): 337-347. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201502013.htm

    Sun G Q, Lü J W, Zhao M J, et al. Diagenesis and sedimentary environment of miocene series in Eboliang Ⅲ area[J]. Acta Sedimentologica Sinica, 2015, 33(2): 337-347(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201502013.htm
    [56] Suess E, Whiticar M J. Methane-derived CO2 in pore fluids expelled from the Oregon subduction zone[J]. Palaeogeography, Palaeoclimatology, Palaoecology, 1989, 97(1/2): 119-136. http://www.sciencedirect.com/science/article/pii/0031018289900333
    [57] 宫文杰, 张振强. 松辽盆地南部泉头组砂岩型铀矿成矿条件分析[J]. 地球学报, 2010, 31(6): 813-818. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201006008.htm

    Gong W J, Zhang Z Q. Metallogenic condition analysis of the sandstone uranium deposit in Quantou Formation, southern Songliao Basin[J]. Acta Geoscientia Sinica, 2010, 31(6): 813-818(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201006008.htm
    [58] 唐振兴, 苗洪波, 李爱民, 等. 松辽盆地南部嫩江组-泉四段油气运移特征[J]. 大庆石油地质与开发, 2007, 26(6): 40-42. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK200706012.htm

    Tang Z X, Miao H B, Li A M, et al. Hydrocarbon migration characteristics of Nenjiang Formation-member 4 of Quantou Formationin southern Songliao Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2007, 26(6): 40-42(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK200706012.htm
    [59] 陈均亮, 林春华, 杭文艳. 大庆长垣构造体系的变形序列及形成机制[J]. 大庆石油地质与开发, 2015, 34(5): 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201505001.htm

    Chen J L, Lin C H, Hang W Y. Deeormation sequence and forming mechanism of the structural system for Daqing placanticline[J]. Petroleum Geology & Oilfield Development in Daqing, 2015, 34(5): 1-6(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201505001.htm
  • 加载中
图(7) / 表(1)
计量
  • 文章访问数:  104
  • HTML全文浏览量:  6
  • PDF下载量:  576
  • 被引次数: 0
出版历程
  • 收稿日期:  2020-08-24

目录

    /

    返回文章
    返回