• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    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

    高演化海相烃源岩元素地球化学评价: 以四川南江杨坝地区下寒武统为例

    曹婷婷 徐思煌 周炼 王约

    曹婷婷, 徐思煌, 周炼, 王约, 2014. 高演化海相烃源岩元素地球化学评价: 以四川南江杨坝地区下寒武统为例. 地球科学, 39(2): 199-209. doi: 10.3799/dqkx.2014.019
    引用本文: 曹婷婷, 徐思煌, 周炼, 王约, 2014. 高演化海相烃源岩元素地球化学评价: 以四川南江杨坝地区下寒武统为例. 地球科学, 39(2): 199-209. doi: 10.3799/dqkx.2014.019
    Cao Tingting, Xu Sihuang, Zhou Lian, Wang Yue, 2014. Element Geochemistry Evaluation of Marine Source Rock with High Maturity: A Case Study of Lower Cambrian in Yangba Section of Nanjiang County, Sichuan. Earth Science, 39(2): 199-209. doi: 10.3799/dqkx.2014.019
    Citation: Cao Tingting, Xu Sihuang, Zhou Lian, Wang Yue, 2014. Element Geochemistry Evaluation of Marine Source Rock with High Maturity: A Case Study of Lower Cambrian in Yangba Section of Nanjiang County, Sichuan. Earth Science, 39(2): 199-209. doi: 10.3799/dqkx.2014.019

    高演化海相烃源岩元素地球化学评价: 以四川南江杨坝地区下寒武统为例

    doi: 10.3799/dqkx.2014.019
    基金项目: 

    中国石化股份有限公司海相油气勘探前瞻性研究项目 G0800-06-ZS-319

    详细信息
      作者简介:

      曹婷婷(1986-), 女, 助理工程师, 主要从事油气成藏方面的研究.E-mail: caotingqi@sina.com

      通讯作者:

      徐思煌, E-mail: xusih@cug.edu.cn

    • 中图分类号: P595

    Element Geochemistry Evaluation of Marine Source Rock with High Maturity: A Case Study of Lower Cambrian in Yangba Section of Nanjiang County, Sichuan

    • 摘要: 评价高演化海相烃源岩已成为国内油气勘探的难点.尝试以四川南江杨坝地区下寒武统烃源岩为例, 利用元素地球化学参数建立高演化海相烃源岩评价的新方法.在计算得到与海洋自生有机质相关的自生元素含量基础上, 通过聚类分析将成因作用相同的自生元素聚为一类, 并建立指示有机质沉积环境及基本属性的参数与自生元素含量之间的线性关系, 从而优选出与有机质富集密切相关的自生元素, 并利用因子分析得到4个反映有机质从形成、沉积到埋藏过程中环境变化的主因子, 最终得到能够反映烃源岩的形成条件优劣的公式.依此对南江杨坝下寒武统烃源岩的品质进行划分.实践证明, 该方法可为高演化海相烃源岩的评价提供一些新思路.

       

    • 图  1  四川南江杨坝地区地理位置及下寒武统地层柱状图

      Fig.  1.  Location and the stratigraphic column of the Lower Cambrian in Yangba area of the Nanjiang County, Sichuan basin

      图  2  各元素含量聚类分析结果

      Fig.  2.  Clustering analysis of element contents

      图  3  杨坝剖面因子分析综合得分及与TOC对照

      Fig.  3.  General factor scores and total organic carbon (TOC) from Yangba section

      表  1  四川盆地南江杨坝地区下寒武统微量元素分析(单位:10-6)

      Table  1.   Element contents of the Lower Cambrian in Yangba area of the Nanjiang County, Sichuan basin

      样品 Al Ba Ca Fe Mg Mn Mo P Sr V Cr Co Ni Ti Cu Zn Pb U
      74-1 18 311.92 718.93 2 310.99 2 6337.88 7 600.06 67.07 24.54 810.15 39.93 2 093.24 173.63 14.84 173.64 3 336.32 87.85 176.20 34.22 11.34
      74-2 57 122.81 912.64 2 885.38 8 952.95 6 614.88 20.81 55.04 257.81 58.30 382.15 82.20 2.17 24.47 3 378.74 27.46 95.85 37.36 24.91
      74-3 40 994.65 858.01 1 708.78 10 410.32 5 812.95 25.49 54.95 323.18 47.48 287.89 122.76 3.66 32.60 3 340.13 28.49 101.81 34.08 25.07
      74-4 56 324.46 918.46 769.07 24 581.74 5 899.68 33.32 53.58 593.60 69.11 349.32 134.54 12.26 72.84 3 368.13 56.46 103.76 32.62 24.72
      74-5 55 272.38 876.66 3 238.46 7 232.46 5 153.79 20.09 24.14 282.99 80.38 732.58 128.38 1.68 32.12 3 596.13 22.73 80.05 33.33 16.05
      75-1 57 414.19 836.68 4 509.22 9 739.08 5 388.70 39.77 27.45 374.95 92.69 607.14 68.99 3.06 39.19 3 299.95 39.50 48.61 29.61 15.63
      75-2 64 456.40 964.24 2 991.06 17 996.97 9 256.53 78.80 19.54 729.36 96.99 319.98 94.05 5.71 27.19 4 065.38 29.63 54.63 35.96 9.85
      75-3 70 171.97 970.45 2 575.92 2 2487.61 7 794.50 77.09 23.08 217.15 104.21 272.93 4 183.46
      76-1 52 129.31 766.52 50 628.92 17 371.01 11 233.02 361.08 2.14 882.92 278.85 202.86 40.74 9.05 32.56 2 598.25 28.89 77.47 23.66 3.26
      76-2 57 501.44 854.39 56 378.93 19 797.91 14 061.61 484.43 4.59 360.14 278.97 176.94 3 161.22
      76-3 59 160.01 657.89 54 135.56 24 533.53 13 087.24 432.77 1.66 297.37 290.89 208.77 3 201.74
      76-4 56 450.49 605.54 58 549.42 22 645.55 13 143.51 401.87 9.73 716.80 331.69 285.13 99.11 12.09 47.25 2 521.45 44.42 98.62 29.32 2.72
      78-1 62 218.59 792.86 58 357.98 24 787.53 15 566.32 464.96 2.11 352.65 309.00 200.66 3 689.52
      78-2 66 023.00 1 251.82 38 017.48 24 466.55 14 560.26 363.74 2.82 448.83 177.20 204.21 86.85 11.33 35.00 4 013.27 23.82 119.83 15.03 2.60
      78-3 55 241.60 768.26 44 170.99 23 978.29 15 677.99 373.26 0.92 818.40 237.53 242.76 123.11 11.95 40.75 3 726.03 32.21 91.92 30.98 2.83
      78-4 55 592.27 1 233.01 30 112.52 24 552.79 15 471.64 322.47 1.11 1 107.54 153.10 245.90 57.12 11.78 45.26 3 858.59 35.29 109.61 34.82 2.93
      79-1 54 717.39 1 032.75 65 307.42 20 005.02 12 458.63 384.04 1.19 1 013.45 285.03 187.46 104.72 9.81 33.63 3 249.72 25.66 76.67 30.42 2.80
      79-2 53 799.53 971.63 46 584.41 19 523.29 14 101.06 331.05 0.38 695.01 201.13 213.33 91.13 9.67 36.46 3 283.30 525.61 80.84 21.24 2.45
      80-1 236.01 4.95 176 037.75 375.13 69 497.90 170.05 0.24 20.69 53.32 2.09 8.34
      80-2 59 323.20 1 010.61 67 342.15 23 347.54 15 211.03 459.92 0.64 326.89 276.28 208.18 94.89 12.75 37.59 3 632.86 22.11 81.31 10.37 2.33
      80-3 63 773.86 954.82 40 135.84 19 992.66 15 197.50 256.16 0.00 800.75 191.22 169.09 88.52 10.35 37.83 3 109.09 26.46 56.13 29.69 3.76
      81-1 56 681.63 711.98 71 083.53 20 987.49 14 962.35 406.16 0.19 744.74 299.72 172.61 93.52 10.10 37.71 2 842.89 28.90 57.78 23.89 2.86
      81-2 56 935.43 856.51 61 284.29 18 872.45 13 084.17 433.95 1.49 370.85 252.75 184.37 3 338.60
      82-1 63 208.65 725.78 33 088.18 24 119.31 15 125.80 398.48 0.85 359.10 171.80 216.80 101.12 12.77 33.48 3 407.09 21.57 119.96 10.80 2.60
      83-1 58 112.68 942.40 9 792.60 9 754.76 4 392.54 31.67 19.03 227.69 90.82 209.79 96.02 2.92 26.88 3 021.73 9.69 71.58 16.96 10.11
      84-1 43 109.77 507.06 4 844.37 26 116.84 8 029.09 1 131.80 1.33 468.94 57.91 171.96 84.92 8.49 36.96 1 765.39 10.40 57.32 6.73 2.64
      85-1 43 927.96 346.49 6 069.88 58 916.35 10 838.91 2 083.94 0.32 980.03 52.01 188.22 67.76 14.33 45.61 1 781.74 13.89 64.68 4.35 2.66
      87-1 61 972.26 592.21 30 982.40 22 305.71 11 883.75 578.07 1.30 418.44 141.23 237.30 80.65 10.08 42.13 2 735.22 24.07 80.42 10.76 2.84
      89-1 76 409.51 651.29 31 199.57 30 816.78 15 021.97 534.94 0.51 431.05 116.67 341.22 130.17 15.23 55.28 3 826.44 41.47 144.24 13.82 3.84
      90-1 66 184.84 804.65 63 227.76 29 257.54 17 091.67 903.76 0.95 411.60 279.63 292.72 114.36 18.78 52.54 3 344.50 31.93 130.53 13.36 3.70
      91-1 58 859.62 737.08 45 105.99 27 189.14 17 881.54 664.57 0.00 979.94 218.98 265.50 89.17 16.88 60.80 3 282.37 46.94 154.52 30.09 3.83
      91-2 72 102.61 620.98 40 704.63 28 151.32 19 596.14 643.86 1.77 418.80 170.92 294.89 125.50 14.17 52.61 3 714.92 41.06 167.37 11.08 3.81
      92-1 71 358.78 614.19 49 854.76 26 277.86 18 132.10 734.60 1.70 387.02 207.70 264.69 120.51 14.90 50.21 3 705.36 32.22 131.18 24.13 3.56
      93-1 53 663.14 549.16 40 388.09 26 986.94 16 760.33 523.36 0.01 1 073.50 162.62 257.71 127.70 15.63 58.28 3 131.69 46.65 101.23 27.39 3.81
      93-2 65 486.26 721.13 39 125.69 27 645.99 14 407.53 499.68 0.91 394.43 171.99 273.45 3 085.42
      94-1 71 812.32 563.59 55 264.39 28 612.82 18 089.83 665.67 0.99 395.21 227.45 288.40 113.53 15.28 51.09 3 425.48 37.65 97.76 85.83 3.62
      95-1 54 634.36 825.56 50 174.07 21 201.51 13 215.59 574.42 1.17 357.66 209.82 213.65 110.85 11.10 35.24 2 796.97 22.24 71.79 9.22 3.04
      96-1 50 843.49 352.92 106 001.54 20 858.46 16 063.63 1 108.38 1.72 919.19 281.34 209.86 87.68 12.56 46.34 2 402.16 28.57 83.13 24.71 5.44
      96-2 53 027.61 356.63 101 835.29 21 138.99 14 219.87 1 036.84 1.20 307.07 276.54 205.96 2 180.76
      97-1 55 159.30 449.73 46 581.49 26 387.24 21 725.80 610.46 0.00 1 024.85 113.40 276.40 115.17 15.80 58.46 3 227.12 60.54 112.34 31.09 4.24
      97-2 39 241.06 442.48 43 178.59 34 751.69 13 209.74 736.98 1.39 488.34 171.64 156.48 1 451.44
      97-3 48 345.59 515.02 38 648.38 42 816.58 14 764.29 705.96 0.51 514.73 123.24 200.25 92.95 37.18 53.08 2 446.57 11.82 71.47 8.12 3.10
      98-1 57 090.22 387.04 58 014.87 21 600.16 16 982.66 692.24 1.03 329.27 151.40 230.51 86.30 11.39 36.24 2 752.53 22.31 78.38 9.04 2.94
      99-1 32 030.56 339.83 119 146.12 11 276.28 10 077.69 709.39 0.10 506.44 252.20 105.14 47.98 5.68 24.40 1 204.77 24.04 93.22 26.81 1.64
      99-2 27 184.69 315.72 121 900.16 9 338.35 8 259.89 750.82 0.69 148.21 234.98 83.60 931.79
      100-1 6 770.10 50.50 308 308.71 6 195.89 5 935.22 2 090.84 0.81 703.17 398.92 28.82 30.26 4.65 10.83 291.82 6.63 23.64 30.84 4.18
      101-1 35 760.31 355.01 79 418.72 11 095.55 11 350.52 417.54 0.75 799.25 151.65 126.44 119.38 7.99 33.97 1 375.54 24.62 60.67 26.46 1.93
      101-2 39 538.18 363.42 81 123.16 13 592.57 9 098.73 449.26 1.63 323.01 154.31 148.96 1 753.42
      102-1 2 813.22 26.92 268 198.64 4 232.58 27 313.19 636.10 0.67 37.56 237.83 9.40 22.26 1.32 5.01 70.97 10.36 49.08 4.34 0.43
      103-1 4 317.48 28.21 324 713.05 3 535.66 21 507.85 471.90 1.00 81.55 298.35 17.07 136.46
      103-2 8 480.69 56.68 278 286.33 4 858.26 20 035.16 458.63 0.41 240.82 358.28 36.05 31.08 2.56 14.54 371.02 36.29 58.40 26.43 1.16
      103-3 2 019.33 31.14 285 574.76 5 339.96 21 895.77 723.55 0.20 59.87 240.47 12.80 96.54
      104-1 16 232.08 1 498.97 195 059.00 6 329.54 9 878.70 381.84 1.04 112.94 254.62 48.61 44.81 2.37 10.37 562.77 26.70 50.43 12.22 0.90
      105-1 20 589.66 126.09 229 374.88 8 252.18 27 529.26 448.51 0.00 276.25 286.48 74.71 46.14 3.53 20.25 869.76 14.95 44.83 26.30 1.04
      106-1 22 341.54 147.36 202 388.72 9 907.26 28 216.31 556.89 0.51 121.17 200.05 77.58 39.66 7.08 21.03 876.74 10.37 25.93 12.76 1.14
      107-1 10 446.32 53.12 195 484.01 4 520.13 16 504.13 338.00 2.45 324.66 272.84 31.88 15.94 2.09 16.61 432.04 17.11 150.28 26.73 1.50
      107-2 12 346.11 61.00 275 538.43 5 010.06 7 542.89 421.81 0.48 134.65 279.98 45.75 37.07 3.02 11.93 503.26 50.70 45.83 7.82 0.84
      108-1 7 837.58 42.39 254 612.25 5 345.90 24 445.81 597.38 1.92 189.96 230.11 27.53 38.78 2.15 20.10 251.23 50.05 104.89 27.71 1.10
      108-2 3 128.77 26.33 262 448.11 4 285.21 36 369.38 1 080.59 0.68 41.48 356.88 12.99 101.74
      111-1 34 765.87 1 537.80 35 589.84 13 485.53 16 873.74 1 696.68 1.29 192.38 119.42 106.63 118.30 5.24 16.90 1 419.81 10.06 42.27 11.45 1.39
      112-1 28 304.77 1 896.47 46 260.31 8 167.04 10 039.90 1 022.13 0.73 235.99 123.94 78.38 63.37 3.30 9.14 1 068.04 16.51 24.14 16.62 1.95
      112-2 71 835.42 573.95 3 419.12 31 134.68 14 302.92 299.70 0.74 340.65 56.92 306.61 3 286.43
      113-1 88 320.71 745.62 4 536.81 33 174.44 17 440.93 344.40 0.48 387.21 40.09 397.24 151.61 13.83 60.28 4 039.31 80.11 136.43 9.69 3.72
      114-1 25 208.55 5 349.92 26 578.95 12 887.44 4 148.49 831.10 1.18 187.22 207.32 87.53 107.20 2.45 11.29 1 305.08 368.25 32.98 8.80 1.03
      115-1 49 948.08 1 943.83 17 998.89 28 777.93 13 249.77 948.27 1.55 313.32 133.34 196.27 73.91 7.53 30.30 2 220.69 34.79 71.20 13.51 2.39
      115-2 51 882.26 1 767.57 4 346.38 13 929.31 7 601.42 291.67 0.97 188.81 93.31 140.60 1 812.62
      116-1 77 523.56 585.46 5 954.79 38 612.82 15 613.05 373.91 0.83 359.77 73.92 334.07 3 918.09
      116-2 36 122.88 1 596.41 9 121.35 14 869.47 4 421.69 582.90 0.87 159.73 106.30 94.06 124.62 11.48 49.26 1 225.81 20.97 115.07 9.90 3.45
      117-1 27 547.03 407.46 1 614.50 3 153.48 1 127.51 74.73 0.78 89.27 41.53 55.59 148.62 1.37 4.89 638.22 7.77 22.45 8.41 0.69
      118-1 42 342.84 487.03 5 821.14 15 163.87 6 609.89 366.78 1.20 242.52 64.40 127.32 52.43 5.68 20.96 1 478.58 99.76 63.13 8.85 1.52
      119-1 36 438.26 410.26 4 190.80 11 316.75 4 528.78 109.23 1.42 481.58 68.61 109.18 106.16 5.59 17.60 1 268.68 25.18 43.51 9.27 1.46
      120-1 27 758.09 386.67 1 985.32 11 443.64 3 581.33 97.15 1.82 169.61 35.31 82.50 157.03 4.22 15.60 1 183.75 7.60 39.53 6.45 1.13
      121-1 45 764.40 588.71 2 941.32 17 258.12 6 555.05 149.79 1.16 225.14 44.83 153.92 54.66 6.99 26.55 2 035.03 6.43 46.61 7.57 2.07
      122-1 48 025.33 601.85 1 858.54 18 505.90 5 438.69 126.88 0.80 169.70 47.27 138.23 1 795.92
      123-1 33 049.74 427.62 13 955.57 14 767.47 9 733.51 258.52 0.91 173.19 55.18 128.93 44.80 5.91 18.48 1 676.33 25.76 37.87 6.85 1.85
      124-1 13 568.25 297.00 1 422.04 10 979.86 2 319.56 213.74 1.41 132.48 22.68 53.92 31.89 2.82 8.92 746.24 10.67 30.27 8.86 0.92
      125-1 35 045.75 1 557.52 10 024.23 17 363.48 4 988.92 128.26 2.24 1 546.34 73.14 98.45 36.23 6.70 19.91 1 198.62 136.93 49.92 7.19 3.20
      125-2 21 951.10 675.46 2 819.16 12 823.45 3 522.35 101.66 0.88 254.69 38.43 72.10 778.41
      125-3 82 439.46 896.26 5 478.86 27 212.28 12 605.86 217.55 1.34 261.53 69.87 261.41 4 083.40
      127-1 43 917.99 532.75 2 515.54 14 944.49 5 763.83 236.63 1.28 211.19 52.45 124.44 116.05 6.73 23.29 1 884.09 8.77 42.68 7.38 1.54
      129-1 95 380.96 730.91 2 839.81 36 304.27 15 174.80 347.09 0.89 215.56 67.93 353.48 123.29 18.28 56.96 4 073.50 49.96 109.06 7.68 3.75
      130-1 6 945.30 350.99 3 036.85 37 474.79 1 158.21 53.62 2.38 508.78 32.89 85.33 33.85 1.64 5.73 411.69 13.61 17.13 4.03 2.19
      130-2 73 839.20 724.93 2 920.21 31 475.62 14 472.81 257.93 0.67 268.17 50.50 269.23 3 907.33
      130-3 8 236.40 797.05 7 591.92 32 250.42 3 659.25 182.15 4.34 1 224.50 74.69 136.78 475.43
      131-1 45 463.72 800.76 1 782.68 23 279.61 11 597.82 176.44 1.07 493.96 36.83 177.42 60.28 10.73 42.47 2 820.29 36.76 73.87 25.99 2.27
      132-1 18 573.41 260.40 62 876.95 5 332.66 31 982.94 259.94 0.33 112.74 51.86 47.50 25.49 1.19 4.13 750.30 6.17 14.12 36.54 1.14
      133-1 19 994.86 266.12 60 471.77 4 607.20 35 124.70 236.76 0.35 270.60 46.14 44.79 96.94 1.52 13.38 1 001.10 15.68 26.66 24.19 1.08
      133-2 5 934.51 59.34 172 391.19 5 923.37 65 845.86 564.51 1.09 22.94 71.66 20.65 31.86 1.66 6.12 168.92 6.14 55.55 14.14 1.42
      134-1 4 477.52 54.12 163 086.18 3 480.67 76 899.24 422.71 0.00 50.51 51.82 10.25 20.11 0.84 11.19 178.08 11.00 24.54 28.36 0.34
      135-1 9 650.35 868.12 168 924.77 6 155.98 67 028.75 520.92 0.40 43.65 69.11 26.90 65.85 1.54 5.78 407.94 7.84 17.23 14.90 0.48
      136-1 5 464.71 47.19 108 038.66 3 099.90 49 593.50 330.46 0.30 28.46 43.57 22.60 37.35 1.40 3.34 207.13 5.72 15.36 7.58 0.98
      137-1 12 612.59 312.16 154 657.10 7 152.78 63 113.29 533.89 0.17 70.25 59.25 48.77 21.34 2.50 9.49 502.82 8.60 22.44 13.79 1.41
      139-1 18 429.21 3 769.75 100 174.55 4 931.22 49 204.81 355.11 1.01 105.03 96.83 43.03 37.28 1.37 4.64 825.44 5.20 35.09 7.84 1.34
      140-1 23 201.78 282.20 47 794.39 5 860.66 28 089.45 190.13 0.79 144.17 34.20 73.19 68.19 2.89 7.17 1 546.64 10.03 20.28 15.70 1.58
      141-1 2 148.20 41.50 185 523.00 3 719.97 70 734.62 447.00 1.23 29.15 66.30 14.08 14.60 0.91 4.08 85.09 5.07 26.12 10.40 1.10
      注:表格中空白处表示无测试数据.
      下载: 导出CSV

      表  2  旋转后的因子载荷矩阵

      Table  2.   Rotated component matrix

      主因子旋转载荷
      1 2 3 4
      Moxs 0.863 0.212 -0.183 0.168
      Uxs 0.855 0.229 -0.169 0.159
      Fexs -0.809 0.171 -0.023 0.183
      Mnxs -0.597 -0.002 0.482 0.338
      Nixs -0.081 0.957 -0.098 -0.027
      Vxs 0.277 0.810 -0.309 0.019
      Znxs 0.074 0.725 0.357 -0.230
      Srxs -0.181 -0.077 0.921 -0.010
      Baxs 0.032 -0.121 0.013 0.886
      注:提取方法:主成分分析法;旋转方法:加入Kaiser常态化的方差最大旋转.
      下载: 导出CSV

      表  3  因子得分系数矩阵

      Table  3.   Component score coefficient matrix

      主因子
      1 2 3 4
      Baxs 0.032 0.011 0.019 0.855
      Fexs -0.399 0.148 -0.222 0.187
      Mnxs -0.156 0.086 0.272 0.328
      Moxs 0.348 0.047 0.072 0.184
      Vxs -0.004 0.350 -0.167 0.082
      Nixs -0.128 0.449 -0.067 0.048
      Znxs 0.078 0.333 0.365 -0.166
      Uxs 0.346 0.056 0.083 0.177
      Srxs 0.159 0.014 0.763 -0.013
      下载: 导出CSV
    • [1] Alberdi-Genolet, M., Toceo, R., 1999. Trace Metals and Organic Geochemistry of the Machiques Member (Aptian-Albian) and La Luna Formation (Cenomanian-Campanian), Venezuela. Chemical Geology, 160: 19-38. doi: 10.1016/S0009-2541(99)00044-3
      [2] Bailey, S.W., Hornbeck, J.W., Priscoll, C.T., et al., 1996. Calcium Inputs and Transport in a Base Poor Forest Ecosystem as Interpreted by Sr Isotopes. Water Resource Res. , 32: 707-719. doi: 10.1029/95WR03642
      [3] Cao, T.T., Xu, S.H., Wang, Y., et al., 2011. Geobiological Conditions for the Formation of the Lower Cambrian Source Rocks in Yangba Area of Nanjiang County in the Sichuan Basin. Oil & Gas Geology, 32(1): 11-16(in Chinese with English abstract). http://d.wanfangdata.com.cn/periodical/syytrqdz201101002
      [4] Chen, H., Xie, X.N., Li, H.J., et al., 2010. Evaluation of the Permian Marine Hydrocarbon Source Rocks at Shangsi Section in Sichuan Province Using Multi-proxies of Paleoproductivity and Paleoredox. Journal of Palaeogeography, 12(3): 324-333(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX201003011.htm
      [5] Chen, Y.J., Deng, J., Hu, G.X., 1996. Environmental Constraints on the Trace Element Contents and Distribution Patterns in Sediment. Geology and Geochemistry, (3): 97-105(in Chinese).
      [6] Clavert, S.E., 1987. Oceanographic Controls on the Accumulation of Organic Matter in Marine Sediments. In: Brook, J., Fleet, A.J., eds., Marine Petroleum Source Rock. Blackwell Scientific Press, London. doi: 10.1144/GSL.SP.1987.026.01.08
      [7] Hu, X.M., Wang, C.S., Li, X.H., 2001. Stable Carbon Isotope Response to Oceanic Anoxic Events. Journal of Chengdu University of Technology, 28(1): 1-6 (in Chinese with English abstract).
      [8] Huang, J.H., Luo, G.M., Bai, X., et al., 2007. The Organic Fraction of the Total Carbon Burial Flux Deduced from Carbon Isotopes across the Permo-Triassic Boundary at Meishan, Zhejiang Province. Earth Science—Journal of China University of Geosciences, 32(6): 767-773(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200706007.htm
      [9] Huang, Y.J., Wang, C.S., Wang, Y.L., 2005. Progress in the Study of Proxies of Paleocean Productivity. Earth Science Frontiers, 12(2): 163-170 (in Chinese with English abstract). http://www.researchgate.net/publication/284372158_Progress_in_the_study_of_proxies_of_paleocean_productivity
      [10] Jones, B.J., Manning, A.C., 1994. Comparison of Geochemical Indices Used for the Interpretation of Palaeoredox Conditions in Ancient Mudstones. Palaeogeography, Palaeoclimatology, Palaeoecology, 111(1-4): 111-129. doi: 10.1016/0009-2541(94)90085-X
      [11] Kuypers, M.M., Pancost, R.D., Jaap, S., et al., 1999. A Large and Abrupt Fall in Atmospheric CO2 Concentration during Cretaceous Times. Nature, 399: 342-345. doi: 10.1038/20659
      [12] Li, H.J., Xie, X.N., Huang, J.H., et al., 2012. Main Factors Controlling the Formation of Excellent Marine Source Rocks in Permian Maokou Formation of Northwest Sichuan, China. Earth Science—Journal of China University of Geosciences, 37(1): 171-180 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201201021.htm
      [13] Liu, S.L., Liu, Y.H., Lin, G., et al., 2006. REE Geochemical Characteristics and Geological Significance of Mudstones from Neogene, Nanpu Sag, Bohai Basin. Geoscience, 20(3): 449-456(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200603012.htm
      [14] Meyers, S.R., Sageman, B.B., Lyons, T.W., 2005. Organic Carbon Burial Rate and the Molybdenum Proxy: Theoretical Framework and Application to Cenomanian-Turonian Oceanic Anoxic Event 2. Paleoceanography, 20: 2002-2020. doi: 10.1029/2004PA001068
      [15] Mi, W.T., Wang, X.L., Feng, Z.Q., et al., 2012. Carbon Isotope Characteristics and the Implication for the Ancient Ocean Evolution of Doushantuo Formation in Weng'an, Guizhou, China. Journal of Chengdu University of Technology (Science & Technology Edition), 39(3): 396-304 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG201203012.htm
      [16] Miller, E.K., Blum, J.D., Friedland, A.J., 1993. Determination of Soil Exchangeable-Cation Loss and Weathering Rates Using Sr Isotope. Nature, 362: 438-441. doi: 10.1038/362438a0
      [17] Taylor, S.R., Mclennan, S.M., 1985. The Continental Crust: It's Composition and Evolution. Blackwell Scientific Press, United States, 25-30. doi: 10.1002/gj.3350210116
      [18] Tenger, Liu, W.H., Xu, Y.C., et al., 2004. The Discussion on Anoxic Environments and Its Geochemical Identifying Indices. Acta Sedimentologica Sinica, 22(2): 365-372 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200402025.htm
      [19] Tenger, Liu, W.H., Xu, Y.C., et al., 2005a. Correlative Study on Parameters of Inorganic Geochemistry and Hydrocarbon Source Rocks Formative Environment. Advance in Earth Science, 20(2): 193-200(in Chinese with English abstract). http://www.researchgate.net/publication/285837325_Correlative_study_on_parameters_of_inorganic_geochemistry_and_hydrocarbon_source_rocks_formative_environment
      [20] Tenger, Liu, W.H., Xu, Y.C., et al., 2005b. Study on Relation between Inorganic Parameters in Marine Deposits and Developmental Environment of Hydrocarbon Source Rocks: Taking Ordos Basin as an Example. Oil & Gas Geology, 26(4): 411-421. (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200504004.htm
      [21] Tenger, Liu, W.H., Xu, Y.C., et al., 2006. Geochemistry Identification of High-Maturity Marine Carbonate Source Rock—An Example from Ordos Basin. Science in China (Series D), 36(2): 167-176(in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JDXG200604005.htm
      [22] Wang, D.R., 2000. The Geochemistry Character of Stable Isotopes of Oil & Gas. Petroleum Industry Press, Beijing (in Chinese).
      [23] Xie, S.C., Yin, H.F., Xie, X.N., et al., 2007. On the Geobiological Evaluation of Hydrocarbon Source Rocks. Earth Science—Journal of China University of Geosciences, 32(6): 727-740(in Chinese with English abstract). http://www.iacademic.info/user-api/na/articleBybaidu?j=61530&a=594556532731777079
      [24] Xu, S.H., Mei, L.F., Yuan, C.P., et al., 2007. Types, Evolution and Pool-Controlling Significance of Pool Fluid Sources in Superimposed Basins: A Case Study from Paleozoic and Mesozoic in South China. Journal of China University of Geosciences, 18(1): 49-59. doi: 10.1016/S1002-0705(07)60018-1
      [25] Zhang, S.C., Wang, R.L., Jin, Z.J., 2006. The Relationship Between the Cambrian-Ordovician High-TOC Source Rock Development and Paleoenvironment Variations in the Tarim Basin, Western China: Carbon and Oxygen Isotope Evidence. Acta Geologica Sinica, 80(3): 459-466(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200603020.htm
      [26] Zhang, Y.G., 2005. Prospection of Petroleum Geochemistry. Petroleum Geology & Experiment, 27(5): 484-489. http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD200505009.htm
      [27] Zhao, Z.H., 1997. The Trace Element Geochemistical Principle. Science Press, Beijing (in Chinese).
      [28] Zhou, L., Zhang, H.Q., Wang, J., et al., 2008. Assessment on Redox Conditions and Organic Burial of Siliciferous Sediments at the Latest Permian Dalong Formation in Shangsi, Sichuan, South China. Journal of China University of Geosciences, 19(5): 496-506. doi: 10.1016/S1002-0705(08)60055-2
      [29] 曹婷婷, 徐思煌, 王约, 等, 2011. 四川盆地南江杨坝地区下寒武统烃源岩形成的地球生物学条件. 石油与天然气地质, 32(1): 11-16. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201101004.htm
      [30] 陈慧, 解习农, 李红敬, 等, 2010. 利用古氧相和古生产力替代指标评价四川上寺剖面二叠系海相烃源岩. 古地理学报, 12(3): 324-333. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201003011.htm
      [31] 陈衍景, 邓健, 胡桂兴, 1996. 环境对沉积物微量元素含量和配分型式的制约. 地质地球化学, (3): 97-105. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ199603008.htm
      [32] 胡修棉, 王成善, 李祥辉, 2001. 大洋缺氧事件的碳稳定同位素响应. 成都理工学院学报, 28(1): 1-6. doi: 10.3969/j.issn.1671-9727.2001.01.001
      [33] 黄俊华, 罗根明, 白晓, 等, 2007. 浙江煤山P/ T之交碳同位素对有机碳埋藏的指示意义. 地球科学——中国地质大学学报, 32(6): 767-773. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200706007.htm
      [34] 黄永建, 王成善, 汪云亮, 2005. 古海洋生产力指标研究进展. 地学前缘, 12(2): 163-170. doi: 10.3321/j.issn:1005-2321.2005.02.018
      [35] 李红敬, 解习农, 黄俊华, 等, 2012. 川西北二叠系茅口组海相优质烃源岩发育控制因素. 地球科学——中国地质大学学报, 37(1): 171-180. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201201021.htm
      [36] 刘士林, 刘蕴华, 林舸, 等, 2006. 渤海湾盆地南堡凹陷新近系泥岩稀土元素地球化学特征及其地质意义. 现代地质, 20(3): 449-456. doi: 10.3969/j.issn.1000-8527.2006.03.013
      [37] 密文天, 王新利, 冯志强, 等, 2012. 贵州瓮安陡山沱组碳同位素特征及古海洋意义. 成都理工大学学报(自然科学版), 39(3): 396-304. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201203012.htm
      [38] 腾格尔, 刘文汇, 徐永昌, 等, 2004. 缺氧环境及地球化学判识标志的探讨——以鄂尔多斯盆地为例. 沉积学报, 22(2): 365-372. doi: 10.3969/j.issn.1000-0550.2004.02.026
      [39] 腾格尔, 刘文汇, 徐永昌, 等, 2005a. 无机地球化学参数与有效烃源岩发育环境的相关研究. 地球科学进展, 20(2): 193-200. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200502008.htm
      [40] 腾格尔, 刘文汇, 徐永昌, 等, 2005b. 海相地层无机参数与烃源岩发育环境的相关研究——以鄂尔多斯盆地为例. 石油与天然气地质, 26(4): 411-421. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200504004.htm
      [41] 腾格尔, 刘文汇, 徐永昌, 等, 2006. 高演化海相碳酸盐烃源岩地球化学综合判识——以鄂尔多斯盆地为例. 中国科学(D辑), 36(2): 167-176. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200602005.htm
      [42] 王大锐, 2000. 油气稳定同位素地球化学. 北京: 石油工业出版社.
      [43] 谢树成, 殷鸿福, 解习农, 等, 2007. 地球生物学方法与海相优质烃源岩形成过程的正演和评价. 地球科学——中国地质大学学报, 32(6): 727-740. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200706002.htm
      [44] 张水昌, Wang, R.L., 金之钧, 等, 2006. 塔里木盆地寒武纪-奥陶纪优质烃源岩沉积与古环境变化的关系: 碳氧同位素新证据. 地质学报, 80(3): 459-466. doi: 10.3321/j.issn:0001-5717.2006.03.020
      [45] 张义纲, 2005. 油气地球化学的若干展望. 石油实验地质, 27(5): 484-489. doi: 10.3969/j.issn.1001-6112.2005.05.010
      [46] 赵振华, 1997. 微量元素地球化学原理. 北京: 科学出版社.
    • 加载中
    图(3) / 表(3)
    计量
    • 文章访问数:  3529
    • HTML全文浏览量:  156
    • PDF下载量:  515
    • 被引次数: 0
    出版历程
    • 收稿日期:  2013-05-06
    • 刊出日期:  2014-02-01

    目录

      /

      返回文章
      返回