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北黄海盆地褶皱分布与成因类型

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文章导航 > 海洋地质与第四纪地质 > 2006 > 26(6): 65-70

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王后金, 梁世荣, 陈强. 北黄海盆地褶皱分布与成因类型[J]. 海洋地质与第四纪地质, 2006, 26(6): 65-70.
引用本文: 王后金, 梁世荣, 陈强. 北黄海盆地褶皱分布与成因类型[J]. 海洋地质与第四纪地质, 2006, 26(6): 65-70.
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WANG Hou-jin, LIANG Shi-rong, CHEN Qiang. DISTRIBUTION AND ORIGIN TYPES OF THE FOLDS IN THE NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 65-70.
Citation: WANG Hou-jin, LIANG Shi-rong, CHEN Qiang. DISTRIBUTION AND ORIGIN TYPES OF THE FOLDS IN THE NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 65-70.
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北黄海盆地褶皱分布与成因类型

  • 1 中国地质大学 资源学院, 武汉 430074;

  • 2 广州海洋地质调查局, 广州 510760

详细信息
    作者简介: 王后金(1972-),男,高级工程师,硕士生,从事海洋地质和油气地质研究

  • 中图分类号: P738

DISTRIBUTION AND ORIGIN TYPES OF THE FOLDS IN THE NORTH YELLOW SEA BASIN

  • 1 Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China;

  • 2 Guangzhou Marine Geologic Survey, Guangzhou 510760, China

    摘要
  • 北黄海盆地为叠置在华北地台上的中新生代断陷盆地,在地史上经受了多期区域构造运动的改造,地层变形强烈,褶皱构造相当发育,分为伸展型、压缩型、重力型和热力型4大成因类型。其中,与张性正断层相关的伸展型褶皱分布范围最广,可进一步划分为牵引褶皱、逆牵引褶皱、滚动褶皱、翘倾褶皱、补偿性挤压背斜和断层-位移褶皱;形成于区域挤压应力场的压缩型褶皱包括非反转挤压褶皱和反转褶皱,在东部和中部坳陷表现明显;重力型褶皱以发育于古潜山之上的披覆背斜比较常见;由岩浆活动引起的热力型褶皱不甚发育,目前仅见于东部坳陷。
    North Yellow Sea basin is a Mesozoic/Cenozoic fault basin superposing on North China platform, which has distorted stratum and well-developed fold structures due to the reconstruction of several structure movements. The folds in the North Yellow Sea basin are mainly classified into four origin types, namely extensional folds, compressional folds, gravitational force folds and thermogene folds. The extensional folds related to normal faults are distributed most widely, which can be further divided into drag folds, reverse-drag folds, rolled folds, compensation squeezed anticlines and fault-displacement folds;the compressional folds including non-reverse squeezed folds and reverse folds are caused by territorial extrusion stress and spread both in the eastern sag and the mid-sag apparently. As a kind of gravitational force folds, buried-hill drape anticlines are quite easily observed in the North Yellow Sea basin, while the thermogene folds only appear in the eastern sag owing to inactive magmation.
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    • 参考文献(5)
  • [1]

    蔡峰.北黄海盆地中新生代沉积环境及特征[J].海洋地质动态,1997(8):1-4.[CAI Feng. Depositional environment and feature of Cenozoic basin in North Yellow Sea[J]. Marine Geology Letters, 1997

    (8):1-4.]

    [2]

    杜旭东,陆克政,漆家福.黄骅坳陷褶皱分类与成因分析[J].石油大学学报自然科学版,1999,23(1):1-6.

    [DU Xu-dong, LU Ke-zheng, QI Jia-fu.The causes and classification of fold in Huanghua Depression[J]. Journal of China University of Petroleum(Edition of Natural Science), 1999, 23(1):1-6.]

    [3]

    姚超,焦贵浩,王同和,等.含油气构造样式[M].北京:石油工业出版社,2004.[YAO Chao, JIAO Gui-hao, WANG Tong-he, et al. Oil Gas Structure Styles in China[M].Beijing:Petroleum Industry Press, 2004.]

    [4]

    陆克政,朱筱敏,漆家福.含气盆地分析[M].石油大学出版社,2001.[LU Ke-zheng, ZHU Xiao-min, QI Jia-fu.Petroliferous Basin Analysis[M]. China University of Petroleum Press, 2001.]

    [5]

    沈华,刘俊,刘建党.贝尔凹陷褶皱构造样式及成因分析[J].中国矿业,2005,14(3):79-11.

    [SHEN Hua, LIU Jun, LIU Jian-dang. Structure styles and origin of fold in Bei'er depression[J].China University of Mining and Technology Press, 2005, 14(3):79-11.]

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出版历程
收稿日期:  2006-03-30
修回日期:  2006-09-30

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