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论地质历史中区域构造沉降史与海平面变化

赵玉光

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文章导航 > 沉积学报  > 1998 >  16(4): 1-7
赵玉光. 论地质历史中区域构造沉降史与海平面变化[J]. 沉积学报, 1998, 16(4): 1-7.
引用本文: 赵玉光. 论地质历史中区域构造沉降史与海平面变化[J]. 沉积学报, 1998, 16(4): 1-7.
shu
Zhao Yuguang. History of Regional Tectonic Subsidence and Sea Level Changes in Geological History[J]. Acta Sedimentologica Sinica, 1998, 16(4): 1-7.
Citation: Zhao Yuguang. History of Regional Tectonic Subsidence and Sea Level Changes in Geological History[J]. Acta Sedimentologica Sinica, 1998, 16(4): 1-7.
shu

论地质历史中区域构造沉降史与海平面变化

  • 中国地质科学院成都地质矿产研究所 成都 610082

详细信息
    作者简介:

    赵玉光 男 34 岁 研究员 沉积地质学

  • 中图分类号: P736.22;P534.46

History of Regional Tectonic Subsidence and Sea Level Changes in Geological History

  • Chengdu Institute of Geology and Mineral Resources,Chengdu Sichuan 610082

    摘要
  • 摘要: 区域构造沉降史和海平面变化是层序地层学中起决定作用的两个主参数。运用“反剥法”。（back-stripping）建立了研究区内泥盆纪至三叠纪盆地构造沉降地球动力学曲线模型，识别出盆地演化从被动大陆边缘、成熟被动大陆边缘、周缘前陆盆地到后造山前陆盆地的演化序列。同时，运用沉积体系域、地震及碳氧同位素信息反演编制了二叠—三叠纪海平面变化轨迹曲线，研究区内海平面变化与全球海平面升降具同步效应，至晚三叠世研究区海平面变化表现为上升趋势，而全球海平面变化总体处于海平面下降阶段，这与前陆挠曲变形和造山俯冲有关。
    Abstract: The history of regional tectonic subsidence and sea level changes are tw o majo r factors of four factors in sequence stratigraphy.The dynamic model of tecto nic subsidence curves from the Devonian to the Triassic in the study area has been reconstructed by the approach of back stripping.The evolution succession of the basin , which is from the passive continental margin, mature passive continental margin, peripheral foreland basin to post orogeny foreland basin, is identified.At the same time, the curves of sea level changes in the Permian and Triassic have been inversed by the inform ation of sedimentary systems tract, seismic section and isotope of carbon and oxygen.The sea level changes in the study area are in synchronism w ith the global sea level changes. The period of sea level rising in the study area lasts to Changxingian Age of Late Permian and the time of sea level falling is Dalong Age of Late Permian.The sea level changes of Late Triassic in the study area are rising and the global sea level chenges is m ainly in falling stage.It is relative to the o rogenic overthrusting.
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    • 参考文献(1)
  • [1] 1 Bond G C, Kominiz M A. Construction of tectonic subsidence curves for the early Paleozoic miogeocline, southern Canadian Rocky M oun- tains: Implications for subsidence mechanisms, age of b reakup, and crustal thinning, GS AB, 1984, 95: 155～173

    2 Perrier R, Q uiblier J.Thickness changes in sedimentary layer du ring compaction history: methods for quantitative evolution.AAPG, Bull. 1974, 58(3): 507～520

    3 D oglioni G. Goldhammer R K.Compaction-induced subsidence in margin of a carbonate platform, Basin earch, 1988, 1(4): 237～246

    4 殷鸿福, 吕 标, 殷鸿福等著, 中国古生物地理学, 北京: 中国地质大 学出版社, 1988.1～22

    5 Posamentier H W, Goldhamer R K.High resolution sequence stratig- raphy-the east Couler Delta, Alberta, J.S edi.Petrol., 1992, 62 (2): 310～317

    6 Van Wagoner J C, M itchum R M, Campion K M, et al. Siliciclastic sequence stratigraphy in well logs, core and outcrop: concepts for high-resolution correlation of time and space. Am.Assoc. Petrol. Geol. M ethods Explor., 1990, 17: 55

    7 S arg J F. Carbonate sequence stratigraphy In: W ilgus C, Hastings B, Ross C.et al. eds S ea-Level Changes: an integrated approach Soc. Econ.Paleontol M ineral Spec. Pupl., 1988, 42: 155～181

    8 Hardenbol J, Vail P R, Ferrer J.In terpreting paleoenvironments, subsidence history and sea-level changes on passive margins from seismic biostratig raphy.26th Int.Geol.Congr.Geology of Continen- tal M argins.O ceanal Acta, 1981, (Supp14): 33～44

    9 Guidish T M, Lerche I, Kendall CGSTC, O' Brien J J.Relationship betw een eustatic sea level changes and basement subsidence.Bull Am Assoc. Petrol. Geol., 1984, 68: 164～177

    10 Haq B U, Hardbol J, Vail P R. The chronology of fluctuating sea level since the Triassic. Science, 1987, 269: 483～489

    11 W iliams D F, Lerche I, Full W E.Isotope ch ronostratigraphy: theo- ry and methods.San Diego, Academic Press, 1988.345 ～366

    12 Lu Yuanfa, Xu Xiaosong, Zhao Yuguang.Sequence Stratigraphy of the T riassic in the M t.Emei-Xiling snow M ountain Area. Beijing China: Geological Publishing House, 1996.12～13

    13 吴应林, 朱洪发, 朱忠发等.中国南方 三叠纪岩 相古理与 成矿作 用.北京: 地质出版社, 1994.43～51
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出版历程
  • 收稿日期:  1997-10-10
  • 修回日期:  1998-03-03
  • 刊出日期:  1998-08-10

目录

    论地质历史中区域构造沉降史与海平面变化

    • 中国地质科学院成都地质矿产研究所 成都 610082
      • 作者简介:

      赵玉光 男 34 岁 研究员 沉积地质学

    • 收稿日期: 1997-10-10
    • 修回日期: 1998-03-03
    • 刊出日期: 1998-08-10

    • 中图分类号: P736.22;P534.46

    摘要: 区域构造沉降史和海平面变化是层序地层学中起决定作用的两个主参数。运用“反剥法”。（back-stripping）建立了研究区内泥盆纪至三叠纪盆地构造沉降地球动力学曲线模型，识别出盆地演化从被动大陆边缘、成熟被动大陆边缘、周缘前陆盆地到后造山前陆盆地的演化序列。同时，运用沉积体系域、地震及碳氧同位素信息反演编制了二叠—三叠纪海平面变化轨迹曲线，研究区内海平面变化与全球海平面升降具同步效应，至晚三叠世研究区海平面变化表现为上升趋势，而全球海平面变化总体处于海平面下降阶段，这与前陆挠曲变形和造山俯冲有关。

    English Abstract

    赵玉光. 论地质历史中区域构造沉降史与海平面变化[J]. 沉积学报, 1998, 16(4): 1-7.
    引用本文: 赵玉光. 论地质历史中区域构造沉降史与海平面变化[J]. 沉积学报, 1998, 16(4): 1-7.
    shu
    Zhao Yuguang. History of Regional Tectonic Subsidence and Sea Level Changes in Geological History[J]. Acta Sedimentologica Sinica, 1998, 16(4): 1-7.
    Citation: Zhao Yuguang. History of Regional Tectonic Subsidence and Sea Level Changes in Geological History[J]. Acta Sedimentologica Sinica, 1998, 16(4): 1-7.
    shu

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