北黄海中、新生代盆地:残留盆地还是叠合盆地?
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North Yellow Sea Meso-Cenozoic Basin: Residual Basin or Superimposed Basin?
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    摘要:

    根据最新调查资料并结合区域构造背景,运用盆地类型分析方法和识别标志,探讨了北黄海中、新生代盆地类型。基于盆地边缘相、沉积减薄、盆地面积和形态、沉积物镜质体反射率等方面的证据,认为现今呈现的北黄海中、新生代盆地不是残留盆地。通过盆地三大构造层的发育、自成体系的含油气系统、边界断裂的多期活动性、中新生代沉积中心的迁移性、不同成盆期具有不同的盆地结构以及两期伸展成盆与一期坳陷成盆的垂向叠置等方面的综合分析,将北黄海中、新生代盆地确定为叠合型盆地。

    Abstract:

    Based on the newest surveying data and combined with the regional tectonic setting, this paper makes a research on the North Yellow Sea Meso-Cenozoic basin type using the analytical method and distinguishing criteria of basin type. Founded on the evidence about basin-margin facies, sediment thinning, area and form of basin, vitrinite reflectance of sediments, etc., the North Yellow Sea Meso-Cenozoic basin presented nowadays isn’t considered a residual basin. By comprehensive analysis of developed three structural layers, petroleum system in their style, polycyclic activities of marginal faults, migration of Meso-Cenozoic sedimentation center, different basin structures in different basining period, and vertical stacking about two terms extension basining and one term depression basining, etc., the North Yellow Sea Meso-Cenozoic basin is made certain the Superimposed basin.

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李文勇.2009.北黄海中、新生代盆地:残留盆地还是叠合盆地?[J].地质学报,83(9):1269-1275.
liwenyong.2009. North Yellow Sea Meso-Cenozoic Basin: Residual Basin or Superimposed Basin?[J]. Acta Geologica Sinica,83(9):1269-1275.

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  • 收稿日期:2009-02-10
  • 最后修改日期:2009-02-10
  • 录用日期:2009-02-10
  • 在线发布日期: 2009-11-05
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