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

黄陵背斜东南缘埃迪卡拉系碳稳定同位素组成特征及有机质发育关系讨论

周鹏 陈孝红 危凯

周鹏, 陈孝红, 危凯. 黄陵背斜东南缘埃迪卡拉系碳稳定同位素组成特征及有机质发育关系讨论[J]. 地质科技通报, 2020, 39(2): 62-73, 93. doi: 10.19509/j.cnki.dzkq.2020.0207
引用本文: 周鹏, 陈孝红, 危凯. 黄陵背斜东南缘埃迪卡拉系碳稳定同位素组成特征及有机质发育关系讨论[J]. 地质科技通报, 2020, 39(2): 62-73, 93. doi: 10.19509/j.cnki.dzkq.2020.0207
Zhou Peng, Chen Xiaohong, Wei Kai. Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei[J]. Bulletin of Geological Science and Technology, 2020, 39(2): 62-73, 93. doi: 10.19509/j.cnki.dzkq.2020.0207
Citation: Zhou Peng, Chen Xiaohong, Wei Kai. Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei[J]. Bulletin of Geological Science and Technology, 2020, 39(2): 62-73, 93. doi: 10.19509/j.cnki.dzkq.2020.0207

黄陵背斜东南缘埃迪卡拉系碳稳定同位素组成特征及有机质发育关系讨论

doi: 10.19509/j.cnki.dzkq.2020.0207
基金项目: 

中国地质调查局地质调查项目“中扬子古生界页岩气基础地质调查” 121201009000150017

中国地质调查局地质调查项目“湘鄂地区页岩气战略选区调查” DD20190109

详细信息
    作者简介:

    周鹏(1982—),男,高级工程师,主要从事区域地质调查工作。E-mail:zhoupeng_01@126.com

  • 中图分类号: P597+.2

Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei

  • 摘要: 通过在黄陵背斜东南缘部署实施的一口页岩气调查井(EYD5),获取了埃迪卡拉系碳同位素参数和相关有机碳数据,建立了该区埃迪卡拉系陡山沱组-灯影组蛤蟆井段碳同位素曲线,在陡山沱组识别出4次负漂移,2次正漂移区间,在灯影组蛤蟆井段识别出1次负漂移,1次正漂移区间,并可在区域范围内有效对比。探讨了该区陡山沱组四段至灯影组蛤蟆井段在区域上的对比标志,明确了该区陡山沱组碳同位素异常与有机碳含量无相关性,碳同位素的正、负漂移区间均可发育富有机质层段,持续的δ13C负值区间对应富有机质页岩层段发育。

     

  • 图 1  研究区域地质简图[11, 26, 38]

    Figure 1.  Geological map of the study area showing the location of Well EYD5

    图 2  EYD5井陡山沱组-灯影组蛤蟆井段典型岩性特征

    a.灯影组蛤蟆井段岩溶角砾岩;b.陡山沱组四段页岩;c.陡山沱组三段砂屑灰岩;d.陡山沱组二段上部含硅磷质结核白云岩;e.陡山沱组二段下部含硅磷质条带页岩;f.陡山沱组一段盖帽白云岩

    Figure 2.  Typical lithologic photos from the Doushantuo Formation to the Hamajing Member of the Dengying Formation in the Well EYD5

    图 3  EYD5井埃迪卡拉系陡山沱组-灯影组δ13C和δ18O值相关性分析

    Figure 3.  Cross-plots of δ13C vs.δ18O from the Doushantuo Formation to the Dengying Formation in the Well EYD5

    图 4  EYD5井埃迪卡拉系陡山沱组综合柱状图

    Figure 4.  Comprehensive column of the Ediacaran Doushantuo Formation in the Well EYD5

    图 5  宜昌地区EYD5井埃迪卡拉系碳同位素同位素曲线划分及对比[10, 17, 29, 40-42]

    Figure 5.  The carbon isotope correlation of the Ediacaran in the Well EYD5, Yichang area, western Hubei

    图 6  黄陵背斜周缘埃迪卡拉系陡山沱组-灯影组蛤蟆井段地层划分对比图(据文献[49]修改)

    Figure 6.  Stratigraphic division and correlation of the Ediacaran Doushantuo Formation-Hamajing Member of the Dengying Formation in the perphery of the Huangling anticline

    表  1  EYD5井埃迪卡拉系δ13C、δ18O值数据分析结果

    Table  1.   The δ13C and δ18O values of the samples in the Ediacaran from the Well EYD5(continues)

    样品 井深/m δ13CPDB/‰ δ18OPDB/‰ 样品 井深/m δ13CPDB/‰ δ18OPDB/‰ 样品 井深/m δ13CPDB/‰ δ18OPDB/‰
    YD5-4H 1 512.2 -3.48 -6.49 YD5-5H 1 511.7 -3.54 -6.57 YD5-5H* 1 511.7 -2.96 -6.17
    YD5-6H 1 511.5 -3.03 -6.08 YD5-7H 1 511.2 -2.94 -6.54 YD5-8H 1 510.9 -2.88 -6.04
    YD5-9H 1 510.7 -2.81 -5.91 YD5-10H 1 510.3 -2.95 -6.63 YD5-11H* 1 510.1 -2.90 -6.53
    YD5-11H 1 510.1 -2.94 -6.55 YD5-12H 1 509.9 -3.09 -6.87 YD5-13H 1 509.5 -2.95 -6.45
    YD5-14H 1 509.2 -2.95 -7.20 YD5-16H 1 508.3 -3.40 -7.03 YD5-17H 1 508.1 -3.28 -6.79
    YD5-19H 1 507.4 -3.67 -6.55 YD5-23H* 1 506.6 -3.33 -5.85 YD5-23H 1 506.6 -3.30 -5.87
    YD5-24H 1 506.2 -3.55 -5.90 YD5-26H 1 505.5 -3.22 -5.96 YD5-28H 1 505.3 -3.23 -5.83
    YD5-29H 1 505.0 -3.75 -6.06 YD5-31H 1 504.7 -3.41 -6.72 YD5-33H 1 504.3 -3.13 -6.69
    YD5-35H* 1 504.0 -3.36 -5.95 YD5-35H 1 504.0 -3.35 -6.01 YD5-37H 1 503.5 -3.55 -6.36
    YD5-39H 1 503.1 -3.35 -6.77 YD5-41H 1 502.7 -3.61 -6.20 YD5-42H 1 502.5 -3.95 -6.68
    YD5-43H 1 502. 2 -3.25 -6.19 YD5-45H 1 501.7 -3.82 -7.08 YD5-46H 1 501.4 -3.94 -7.05
    YD5-47H 1 501.1 -4.76 -6.30 YD5-49H* 1 500.8 -1.20 -5.29 YD5-49H 1 500.8 -1.21 -5.29
    YD5-50H 1 500.6 -2.17 -7.01 YD5-51H 1 500.1 -1.06 -7.20 YD5-52H 1 499.9 -1.13 -7.27
    YD5-53H 1 499.4 -1.01 -7.12 YD5-54H 1 499.1 -1.35 -7.23 YD5-55H 1 498.5 -0.82 -6.98
    YD5-56H 1 498.0 -1.78 -8.39 YD5-56H* 1 498.0 -1.87 -8.46 YD5-57H 1 497.2 -2.47 -6.67
    YD5-58H 1 496.8 -3.57 -6.21 YD5-59H 1 496.4 -1.74 -5.30 YD5-60H 1 495.8 -4.27 -5.98
    YD5-61H 1 494.9 -0.52 -6.09 YD5-62H 1 494.6 0.11 -5.53 YD5-63H 1 494.4 -0.04 -7.47
    YD5-63H* 1 494.4 -0.08 -7.31 YD5-76H 1 485.3 -1.50 -10.72 YD5-81H 1 481.1 -1.85 -11.40
    YD5-84H 1 478.8 -1.42 -9.82 YD5-86H 1 477.4 -1.52 -11.19 YD5-89H 1 475.2 -2.11 -10.96
    YD5-91H 1 474.0 -1.02 -9.60 YD5-91H* 1 474.0 -1.09 -9.70 YD5-93H 1 473.1 -0.34 -7.93
    YD5-99H 1 470.3 0.83 -4.15 YD5-100H 1 469.6 0.74 -2.71 YD5-100H* 1 469.6 0.74 -2.60
    YD5-102H 1 468.8 1.46 -2.45 YD5-103H 1 468.0 0.30 -2.53 YD5-105H 1 466.8 0.05 -5.02
    YD5-107H 1 466.0 -0.60 -5.17 YD5-107H* 1 466.0 -0.64 -5.25 YD5-109H 1 465.1 0.39 -5.50
    YD5-110H 1 464.1 1.70 -4.46 YD5-112H 1 462.9 2.54 -4.75 YD5-114H 1 461.8 3.09 -4.68
    YD5-117H 1 460.1 1.09 -4.06 YD5-119H 1 458.5 3.02 -4.29 YD5-121H 1 457.1 3.96 -3.90
    YD5-122H 1 456.0 4.51 -4.63 YD5-125H 1 454.6 4.42 -3.88 YD5-126H 1 453.6 3.66 -4.45
    YD5-128H 1 452.5 2.10 -4.33 YD5-128H* 1 452.5 2.16 -4.20 YD5-129H 1 451.6 0.97 -5.82
    YD5-130H 1 450.5 4.14 -6.08 YD5-131H 1 450.0 4.84 -4.56 YD5-132H 1 448.8 4.58 -5.31
    YD5-133H 1 448.1 5.02 -5.31 YD5-133H* 1 448.1 5.02 -5.29 YD5-134H 1 447.6 5.95 -2.53
    YD5-135H 1 446.9 4.96 -3.28 YD5-136H 1 446.0 4.95 -3.17 YD5-137H 1 444.8 5.06 -2.94
    YD5-138H 1 444.0 5.46 -3.57 YD5-139H 1 443.3 5.33 -3.71 YD5-140H 1 442.6 5.53 -4.22
    YD5-140H* 1 442.6 5.62 -4.13 YD5-141H 1 441.5 5.63 -3.57 YD5-142H 1 440.5 5.25 -4.40
    YD5-142H* 1 440.5 5.19 -4.29 YD5-143H 1 439.6 5.02 -5.02 YD5-144H 1 438.5 5.21 -4.77
    YD5-145H 1 437.5 5.32 -4.83 YD5-146H 1 436.7 5.28 -4.56 YD5-147H 1 435.6 5.27 -4.86
    YD5-148H 1 434.5 5.42 -4.24 YD5-149H 1 433.8 5.30 -4.40 YD5-150H 1 432.9 5.63 -3.67
    YD5-151H 1 431.9 5.40 -4.27 YD5-151H* 1 431.9 5.38 -4.29 YD5-152H 1 431.2 6.37 -3.29
    YD5-154H 1 429.4 5.62 -3.44 YD5-156H 1 427.9 5.68 -3.04 YD5-157H 1 426.9 5.73 -2.77
    YD5-158H 1 425.9 6.17 -2.78 YD5-159H 1 424.9 6.08 -2.45 YD5-161H 1 422.6 5.66 -2.63
    YD5-161H* 1 422.6 5.61 -2.63 YD5-162H 1 421.7 5.83 -2.16 YD5-163H 1 420.8 5.98 -2.08
    YD5-165H 1 418.9 5.86 -2.33 YD5-167H 1 417.7 6.90 -2.07 YD5-168H 1 416.1 5.77 -2.27
    YD5-170H 1 414.3 6.33 -2.70 YD5-171H 1 413.5 6.11 -4.17 YD5-171H* 1 413.5 6.22 -4.05
    YD5-172H 1 412.1 5.09 -4.46 YD5-173H 1 411.2 6.09 -4.49 YD5-174H 1 409.7 5.76 -4.29
    YD5-175H 1 409.0 6.10 -4.36 YD5-176H 1 407.7 5.98 -3.37 YD5-177H 1 406.1 5.53 -3.21
    YD5-179H 1 404.5 6.41 -2.61 YD5-180H 1 403.5 5.72 -3.42 YD5-181H 1 402.1 4.67 -2.37
    YD5-181H* 1 402.1 4.64 -2.35 YD5-183H 1 400.1 6.55 -2.43 YD5-184H 1 398.7 5.42 -3.21
    YD5-184H* 1 398.7 5.36 -3.16 YD5-185H 1 397.4 6.34 -3.56 YD5-186H 1 396.4 5.96 -4.55
    YD5-187H 1 395.8 5.61 -4.14 YD5-187H* 1 395.8 5.60 -4.32 YD5-189H 1 394.2 5.92 -4.14
    YD5-190H 1 393.2 6.03 -3.94 YD5-191H 1 391.9 5.70 -4.09 YD5-192H 1 390.1 5.92 -3.70
    YD5-193H 1 388.2 6.46 -3.38 YD5-195H 1 387.2 6.19 -2.81 YD5-196H 1 386.3 6.22 -2.58
    YD5-197H 1 385.2 6.09 -2.48 YD5-198H 1 383.3 6.38 -2.45 YD5-198H* 1 383.3 6.45 -2.53
    YD5-200H 1 381.5 6.67 -2.14 YD5-201H 1 380.2 5.18 -3.11 YD5-202H 1 378.4 6.01 -2.46
    YD5-203H 1 376.8 5.83 -2.43 YD5-204H 1 375.5 5.96 -2.68 YD5-205H 1 373.9 6.21 -2.33
    YD5-205H* 1 373.9 6.34 -2.30 YD5-206H 1 372.4 6.53 -2.18 YD5-207H 1 371.2 5.71 -2.87
    YD5-208H 1 369.9 5.66 -2.42 YD5-209H 1 367.9 5.57 -2.82 YD5-210H 1 366.3 5.60 -2.84
    YD5-210H* 1 366.3 5.54 -2.89 YD5-211H 1 364.8 5.46 -2.46 YD5-212H 1 363.7 4.99 -2.48
    YD5-213H 1 362.2 5.56 -2.27 YD5-214H 1 360.8 5.15 -2.45 YD5-215H 1 359.2 4.40 -2.49
    YD5-216H 1 357.1 5.60 -2.69 YD5-217H 1 355.9 5.09 -2.02 YD5-217H* 1 355.9 5.08 -1.97
    YD5-218H 1 354.6 4.63 -2.42 YD5-220H 1 351.4 4.69 -3.34 YD5-221H 1 350.0 5.21 -3.02
    YD5-222H 1 348.6 5.12 -2.82 YD5-223H 1 347.5 5.07 -2.69 YD5-224H 1 346.0 4.97 -2.72
    YD5-225H 1 344.5 5.58 -2.84 YD5-226H 1 342.9 5.19 -1.83 YD5-227H 1 342.6 5.00 -2.03
    YD5-227H* 1 342.6 4.91 -2.19 YD5-228H 1 341.7 5.44 -2.93 YD5-229H 1 340.1 5.78 -3.24
    YD5-230H 1 338.7 6.39 -1.41 YD5-231H 1 337.1 5.90 -2.98 YD5-232H 1 335.8 5.73 -2.88
    YD5-233H 1 333.8 5.96 -2.00 YD5-234H 1 332.7 5.14 -3.90 YD5-235H 1 331.0 5.59 -3.77
    YD5-236H 1 329.8 6.15 -2.93 YD5-236H* 1 329.8 6.21 -3.05 YD5-237H 1 328.2 6.59 -2.18
    YD5-238H 1 326.7 5.86 -2.97 YD5-239H 1 324.7 6.40 -2.30 YD5-241H 1 323.1 3.95 -1.31
    YD5-242H 1 321.5 2.15 -1.23 YD5-243H 1 320.6 4.92 -6.41 YD5-244H 1 319.7 4.41 -6.59
    YD5-245H 1 318.5 6.11 -7.16 YD5-246H 1 317.0 6.67 -6.84 YD5-247H 1 315.2 5.22 -6.51
    YD5-248H 1 313.1 6.29 -6.48 YD5-249H 1 310.9 6.69 -7.27 YD5-250H 1 309.9 6.90 -7.58
    YD5-251H 1 308.3 6.83 -8.50 YD5-252H 1 306.9 7.03 -7.32 YD5-252H* 1 306.9 6.89 -7.53
    YD5-253H 1 305.2 6.29 -8.80 YD5-254H 1 303.6 6.12 -8.78 YD5-255H 1 301.9 6.29 -7.72
    YD5-255H* 1 301.9 6.27 -7.71 YD5-256H 1 300.6 6.95 -2.78 YD5-257H 1 299.5 7.08 -3.61
    YD5-258H 1 297.6 7.09 -4.39 YD5-259H 1 295.2 5.76 -5.97 YD5-260H 1 293.1 4.78 -5.84
    YD5-261H 1 291.4 4.20 -6.02 YD5-262H 1 290.4 3.69 -4.93 YD5-263H 1 289.7 4.07 -2.96
    YD5-263H* 1 289.7 4.09 -2.94 YD5-264H 1 289.0 3.19 -1.74 YD5-266H 1 286.9 4.02 -2.32
    YD5-267H 1 285.4 2.65 -3.95 YD5-268H 1283.9 2.39 -2.33 YD5-269H 1 282.3 1.38 -0.94
    YD5-271H 1 279.7 0.08 -0.61 YD5-271H* 1 279.7 0.02 -0.65 YD5-273H 1 278.6 -0.99 -0.68
    YD5-274H 1 277.0 -1.62 -0.54 YD5-275H 1 275.4 -1.25 -1.69 YD5-277H 1 273.3 -0.67 -1.31
    YD5-279H 1 272.2 -1.24 -2.03 YD5-280H 1 271.1 0.08 -0.41 YD5-282H 1 269.6 1.82 -0.91
    YD5-283H 1 268.3 2.09 -0.56 YD5-283H* 1 268.3 2.07 -0.61 YD5-284H 1 267.7 2.00 -1.09
    YD5-286H 1 266.0 1.46 -1.71 YD5-288H 1 264.4 2.96 -1.74 YD5-290H 1 262.9 3.54 -1.87
    YD5-292H 1 261.7 2.79 -1.43 YD5-294H 1 260.2 4.12 -1.29 YD5-296H 1 258.7 4.68 -3.37
    YD5-297H 1 257.4 4.22 -3.45 YD5-299H 1 255.7 5.56 -1.52 YD5-299H* 1 255.7 5.56 -1.61
    YD5-301H 1 254.6 5.79 -2.31 YD5-302H 1 252.7 5.49 -2.62 YD5-303H 1 251.5 5.40 -1.45
    YD5-303H* 1 251.5 5.44 -1.34 YD5-304H 1 249.2 5.55 -3.97 YD5-305H 1 248.2 5.40 -2.32
    YD5-306H 1 246.9 5.07 -3.03 YD5-307H 1 246.2 4.90 -2.37 YD5-309H 1 245.1 5.76 -1.21
    YD5-310H 1 243.9 5.08 -3.63 YD5-312H 1 242.7 5.43 -2.69 YD5-312H* 1 242.7 5.43 -2.68
    YD5-314H 1 241.3 6.50 -5.46 YD5-316H 1 239.6 6.64 -2.68 YD5-317H 1 238.7 7.19 -5.79
    YD5-319H 1 236.4 5.12 -3.89 YD5-321H 1 234.5 4.88 -4.23 YD5-322H 1 233.2 4.08 -5.60
    YD5-324H 1 232.2 4.99 -3.97 YD5-326H 1 231.1 5.10 -5.97 YD5-328H 1 230.0 4.84 -6.14
    YD5-328H* 1 230.0 4.91 -6.05 YD5-330H 1 228.7 4.61 -5.74 YD5-332H 1 227.1 2.78 -6.14
    YD5-333H 1 226.2 -0.87 -5.56 YD5-334H 1 225.3 -1.60 -4.85 YD5-336H 1 223.9 4.52 -6.61
    YD5-337H 1 222.9 1.62 -3.67 YD5-339H 1 221.7 -4.57 -7.46 YD5-339H* 1 221.7 -4.43 -7.33
    YD5-340H 1 221.0 1.51 -7.52 YD5-341H 1 220.0 0.93 -8.20 YD5-342H 1 217.3 1.83 -5.38
    YD5-343H 1 213.3 2.63 -4.04 YD5-344H 1 209.6 2.85 -3.16 YD5-345H 1 206.9 5.16 -3.04
    YD5-346H 1 205.9 5.77 -4.59 YD5-347H 1 205.0 7.13 -6.11 YD5-348H 1 204.4 7.56 -5.40
    YD5-349H 1 204.4 7.58 -5.48 YD5-350H 1 200.1 7.90 -3.69
    *为重复样
    下载: 导出CSV

    表  2  EYD5井埃迪卡拉系样品有机碳分析结果

    Table  2.   TOC values of samples from the Ediacaran in the Well EYD5

    送样号 深度/m w(TOC)/% 送样号 深度/m w(TOC)/%
    YD5-341H 1220.7 2.17 YD5-113H 1220.7 1.62
    YD5-335H 1224.9 0.86 YD5-108H 1224.9 2.02
    YD5-329H 1229.6 0.52 YD5-104H 1229.6 0.76
    YD5-325H 1231.8 0.36 YD5-98H 1231.8 0.21
    YD5-320H 1235.6 0.28 YD5-94H 1235.6 1.20
    YD5-313H 1242.2 0.30 YD5-90H 1242.2 1.24
    YD5-308H 1245.6 0.28 YD5-85H 1245.6 1.26
    YD5-295H 1259.6 0.28 YD5-82H 1259.6 1.26
    YD5-289H 1263.6 0.42 YD5-79H 1263.6 1.20
    YD5-285H 1266.7 0.35 YD5-77H 1266.7 1.15
    YD5-278H 1272.8 2.05 YD5-73H 1272.8 1.74
    YD5-272H 1279.0 0.89 YD5-70H 1279.0 1.12
    YD5-265H 1288.3 0.77 YD5-65H 1288.3 3.48
    YD5-219H 1351.9 1.78 YD5-64H 1351.9 2.29
    YD5-194H 1387.6 2.16 YD5-48H 1387.6 0.20
    YD5-182H 1401.2 1.53 YD5-40H 1401.2 0.21
    YD5-169H 1415.3 1.64 YD5-36H 1415.3 0.22
    YD5-164H 1419.6 1.45 YD5-32H 1419.6 0.26
    YD5-155H 1428.7 1.68 YD5-27H 1428.7 0.24
    YD5-127H 1453.1 1.16 YD5-22H 1453.1 0.23
    YD5-123H 1455.7 1.97 YD5-20H 1455.7 0.23
    YD5-118H 1459.1 1.76 YD5-15H 1459.1 0.19
    下载: 导出CSV
  • [1] Mcfadden K A, Huang J, Chu X, et al.Pulsed oxidation and bioloical evolution in the Ediacaran Doushantuo Formation[J].Proceedings of the National Academy of Sciences of the United States of America, 2008, 105(9):3197-3202. doi: 10.1073/pnas.0708336105
    [2] 刘鹏举, 尹崇玉, 唐烽, 等.瓮安生物群中后生动物化石研究进展及问题讨论[J].地质论评, 2007, 53(6):728-735. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200706006
    [3] Zhu M, Strauss H, Shields G A.From snowball earth to the Cambrian bioradiation:Calibration of Ediacaran:Cambrian earth history in South China[J].Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 254(1/2):1-6. http://www.sciencedirect.com/science/article/pii/S0031018207001721
    [4] Zhu M, Zhang J, Yang A.Integrated Ediacaran (Sinian) chronostratigraphy of South China[J].Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 254(1/2):7-61. http://www.sciencedirect.com/science/article/pii/S0009254106004207
    [5] 王自强, 尹崇玉, 高林志, 等.用化学地层学研究新元古代地层划分和对比[J].地学前缘, 2006, 13(6):268-279. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200606030
    [6] 陈寿铭, 尹崇玉, 刘鹏举, 等.峡东地区埃迪卡拉系陡山沱组碳同位素特征研究进展与国内外对比[J].地球学报, 2009, 30(4):475-486. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200904008
    [7] 吕苗, 朱茂炎, 赵美娟.湖北宜昌茅坪泗溪剖面埃迪卡拉系岩石地层和碳同位素地层研究[J].地层学杂志, 2009, 33(4):359-372. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200904003
    [8] 蒋干清, 张世红, 史晓颖, 等.华南埃迪卡拉纪陡山沱盆地氧化界面的迁移与碳同位素异常[J].中国科学:地球科学, 2008, 38(12):1481-1495. http://www.cnki.com.cn/Article/CJFDTotal-jdxk200812002.htm
    [9] Jiang G, Wang X, Shi X, et al.Organic carbon isotope constraints on the dissolved organic carbon (DOC) reservoir at the Cryogenian:Ediacaran transition[J].Earth and Planetary Science Letters, 2010, 299(1/2):159-168. http://www.sciencedirect.com/science/article/pii/S0012821X10005431
    [10] 周鹏, 张保民, 陈孝红.湖北宜昌樟村坪埃迪卡拉系陡山沱组C同位素变化及成因[J].地质通报, 2017, 36(5):780-791. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201705010
    [11] 陈孝红, 周鹏, 张保民, 等.峡东埃迪卡拉系陡山沱组稳定碳同位素记录及其年代地层意义[J].中国地质, 2015, 42(1):207-223. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi2015010017
    [12] 陈寿铭, 尹崇玉, 刘鹏举, 等.湖北峡东地区牛坪剖面埃迪卡拉系碳同位素组成及地质意义[J].世界地质, 2013, 32(4):641-651. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sjdz201304001
    [13] 王家生, 甘华阳, 魏清, 等.三峡"盖帽"白云岩的碳、硫稳定同位素研究及其成因探讨[J].现代地质, 2005, 19(1):14-20. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz200501002
    [14] 陈孝红, 李华芹, 陈立德, 等.三峡地区震旦系碳酸盐岩碳氧同位素特征[J].地质论评, 2003, 49(1):66-73. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200301010
    [15] 王伟, 松本良, 王海峰, 等.长江三峡地区上震旦统稳定同位素异常及地层意义[J].微体古生物学报, 2002(4):382-388. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=wtgswxb200204005
    [16] 尹崇玉, 刘鹏举, 陈寿铭, 等.峡东地区埃迪卡拉系陡山沱组疑源类生物地层序列[J].古生物学报, 2009, 48(2):146-154. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gswxb200902003
    [17] 刘鹏举, 尹崇玉, 高林志, 等.湖北宜昌樟村坪埃迪卡拉系陡山沱组微体化石新材料及锆石SHRIMP U-Pb年龄[J].科学通报, 2009, 54(6):774-780. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb200906013
    [18] 刘鹏举, 尹崇玉, 陈寿铭, 等.埃迪卡拉纪陡山沱期瓮安生物群中磷酸盐化球状化石新材料及其问题讨论[J].地球学报, 2009, 30(4):457-464. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200904006
    [19] 唐烽, 尹崇玉, 刘鹏举, 等.华南伊迪卡拉纪"庙河生物群"的属性分析[J].地质学报, 2008(5):601-611. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200805004
    [20] 柳永清, 尹崇玉, 高林志, 等.峡东震旦系层型剖面沉积相研究[J].地质论评, 2003, 49(2):187-194. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200302011
    [21] 李勇.上扬子区晚震旦世地层古生物研究[D].西安: 西北大学, 2002.
    [22] 王自强, 高林志, 尹崇玉.峡东地区震旦系等时层序地层格架的建立[J].中国区域地质, 2001, 20(4):368-376. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200104007
    [23] 王自强, 高林志, 尹崇玉.峡东地区震旦系层型剖面的界定与层序划分[J].地质论评, 2001, 47(5):449-458. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200105001
    [24] 赵自强, 邢裕盛, 丁启秀, 等.湖北震旦系[M].武汉:中国地质大学出版社, 1988.
    [25] 丁莲芳, 李勇, 胡夏嵩, 等.震旦纪庙河生物群[M].北京:地质出版社, 1996:221.
    [26] Wang X, Erdtmann B, Chen X.Integrated sequence-, bio-and chemostratigraphy of the terminal Proterozoic to Lowermost Cambrian "black rock series" from central South China[J].Episodes, 1998, 21(3):178-189. doi: 10.18814/epiiugs/1998/v21i3/007
    [27] 安志辉, 童金南, 叶琴, 等.峡东青林口地区新元古代地层序列及沉积演变[J].地球科学:中国地质大学学报, 2014(7):795-806. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201407004
    [28] An Z, Jiang G, Tong J, et al.Stratigraphic position of the Ediacaran Miaohe biota and its constrains on the age of the Upper Doushantuo δ13C anomaly in the Yangtze Gorges area, South China[J].Precambrian Research, 2015, 271:243-253. doi: 10.1016/j.precamres.2015.10.007
    [29] Zhu M, Lu M, Zhang J, et al.Carbon isotope chemostratigraphy and sedimentary facies evolution of the Ediacaran Doushantuo Formation in western Hubei, South China[J].Precambrian Research, 2011, 225:7-28. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=213f790fb971ba1a0a00197f42eb758e
    [30] 李儒峰, 刘本培.碳氧同位素演化与碳酸盐岩层序地层学关系研究[J].地球科学:中国地质大学学报, 1996, 21(3):29-34. http://www.cnki.com.cn/Article/CJFDTotal-DQKX603.004.htm
    [31] 陈锦石, 闻传芬, 钟华, 等.古生代海洋碳同位素演化[J].地质科学, 1995, 30(4):338-347. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199500062010
    [32] 王可法.海相碳酸盐碳同位素组成及其意义[J].地质地球化学, 1994, 22(5):50-54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400053983
    [33] 陈锦石, 钟华.碳同位素地层学研究[J].矿物岩石地球化学通讯, 1990, 9(2):113-114. http://www.cnki.com.cn/Article/CJFDTotal-KYDH199002009.htm
    [34] 王秋良, 袁胜元, 李长安.江汉平原江陵剖面有机碳含量、碳同位素和磁化率的古气候意义[J].地质科技情报, 2006, 25(4):59-62. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200604011
    [35] 王传尚, 李旭兵, 刘安, 等.华南埃迪卡拉系斜坡相带碳稳定同位素特征[J].地质科技情报, 2014, 33(4):1-5. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201404001
    [36] 陈践发, 张水昌, 鲍志东, 等.海相优质烃源岩发育的主要影响因素[J].海相油气地质, 2006, 11(3):49-54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hxyqdz200603008
    [37] 彭花明, 郭福生, 严兆彬, 等.浙江江山震旦系碳同位素异常及其地质意义[J].地球化学, 2006, 35(6):577-585. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqhx200606001
    [38] Xiaofeng W, Daquan M, Xiaohong C.Precambrian Geological Evolution in the Yangtze Gorges Area, China[J].Gondwana Research, 1999, 2(4):621-626. doi: 10.1016/S1342-937X(05)70223-9
    [39] Kaufman A, Knoll A.Neoproterozoic variations in the C-isotopic composition of seawater:stratigraphic and biogeochemical implications[J].Precambrian Research, 1995, 73:27-49. doi: 10.1016/0301-9268(94)00070-8
    [40] Zhou C, Xiao S.Ediacaranδ13C chemostratigraphy of South China[J].Chemical Geology, 2007, 237:89-108. doi: 10.1016/j.chemgeo.2006.06.021
    [41] Barfod G H, Albaréde F, Knoll A H, et al.New Lu-Hf and Pb-Pb age constraints on the earliest animal fossils[J].Earth Planetary Science Letters, 2002, 201(1):203-212. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=85e181b32833edd021091cfbad1cab63
    [42] Condon D, Zhu M Y, Bowring S, et al.U-Pb ages from the Neoproterozoic Doushantuo Formation, China[J].Science, 2005, 308:95-98. doi: 10.1126/science.1107765
    [43] 蒋干清, 史晓颖, 张世红.甲烷渗漏构造、水合物分解释放与新元古代冰后期盖帽碳酸盐岩[J].科学通报, 2006, 51(10):1121-1138. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb200610001
    [44] 王新强, 史晓颖.华南伊迪卡拉纪碳同位素时空变化及其对生物演化的影响[J].中国科学:地球科学, 2010, 40(1):18-27. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK201000131365
    [45] 李超, 程猛, Algeo Thomas J, 等.早期地球海洋水化学分带的理论预测[J].中国科学:地球科学, 2015, 45(12):1829-1838. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201512004
    [46] Jiang G, Shi X, Zhang S, et al.Stratigraphy and paleogeography of the Ediacaran Doushantuo Formation (ca.635-551 Ma) in South China[J].Gondwana Research, 2011, 19(4):831-849. doi: 10.1016/j.gr.2011.01.006
    [47] Mcfadden K A, Xiao S, Zhou C, et al.Quantitative evaluation of the biostratigraphic distribution of acanthomorphic acritarchs in the Ediacaran Doushantuo Formation in the Yangtze Gorges area, South China[J].Precambrian Research, 2009, 173:170-190. doi: 10.1016/j.precamres.2009.03.009
    [48] 安志辉, 童金南, 叶琴, 等.湖北宜昌樟村坪地区陡山沱组地层划分与对比[J].地球科学, 2018, 43(7):2206-2221. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201807002
    [49] 刘鹏举, 尹崇玉, 陈寿铭, 等.华南峡东地区埃迪卡拉(震旦)纪年代地层划分初探[J].地质学报, 2012, 86(6):849-866. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201206001
    [50] Jiang G, Kaufman A J, Christie-Blick N, et al.Carbon isotope variability across the Ediacaran Yangtze platform in South China:Implications for a large surface-to-deep ocean δ13C gradient[J].Earth and Planetary Science Letters, 2007, 261(1/2):303-320.
    [51] 廖晓, 王震亮, 余侏宇, 等.塔里木地柯坪地区奥陶系高丰度海相烃源岩成因探讨[J].地质科技情报, 2018, 37(2):59-64. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201802008
    [52] Demaison G J, Moore G T.Anoxic environments and oils source bed genesis[J].Organic Geochemistry, 1980, 2(1):9-31. http://aapgbull.geoscienceworld.org/content/64/8/1179
    [53] Tyson R V, Pearson T H.Modern and ancient contiental shelf anoxia[J].Geological Society of Special Publication, 1991, 58:470-482. http://adsabs.harvard.edu/abs/1991gslsp..58..187r
    [54] 腾格尔.海相地层元素-碳氧同位素分布与沉积环境和烃源岩发育关系: 以鄂尔多斯盆地为分例[D].兰州: 中国科学院兰州地质研究所, 2004. http://cdmd.cnki.com.cn/Article/CDMD-80053-2004102000.htm
    [55] 王大锐, 白玉雷.碳酸盐岩中稳定同位素对古气候的表征[J].石油勘探与开发, 1999, 26(5):30-32. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199901060806
    [56] 周新科, 许化政.海相碳酸盐岩的形成环境与有机质特征[J].石油与天然气地质, 2009, 30(3):337-342, 349. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz200903013
    [57] 严兆彬, 郭福生, 潘家永, 等.碳酸盐岩C, O, Sr同位素组成在古气候、古海洋环境研究中的应用[J].地质找矿论丛, 2005, 20(1):53-56. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzzklc200501010
  • 加载中
图(6) / 表(2)
计量
  • 文章访问数:  317
  • PDF下载量:  729
  • 被引次数: 0
出版历程
  • 收稿日期:  2019-06-29

目录

    /

    返回文章
    返回