江汉盆地西北部断陷带构造变形分析与古应力场演化序列
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中国地质科学院地质力学研究所基本科研项目


Tectonic Deformation Analysis and Paleostress Field Sequence of the Grabens
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    摘要:

    江汉盆地内部发育多个断陷带,其形成与演化对盆地油气聚集至关重要。本文以远安和南漳断陷带为重点,基于详细的野外观察和断裂变形测量,分析了江汉盆地西北部断陷带的构造变形特征,建立了盆地古构造应力场演化序列。结合区域构造分析与变形叠加特征研究,将断陷带白垩纪以来的构造演化历史划分为4个阶段:①晚白垩世-古近纪,受NEE-SWW向引张作用,江汉盆地内部发生断陷;②古近纪末期,断陷盆地遭受近E-W向挤压作用而发生构造反转;③新近纪,先后受NE-SW向引张和NW-SE向引张作用,断陷带再次伸展沉降;④新近纪末期,在NE-SW向构造挤压作用下,断陷带发生右旋走滑活动。江汉盆地晚白垩世以来构造变形序列的建立,为探讨江汉盆地后期构造演化及油气成藏改造提供了构造地质学证据。

    Abstract:

    There are several grabens in Jianghan Basin, which are essential to oil and gas reconstruction. Based on detailed observation of tectonic deformation in both Yuan’an Graben and Nanzhang Graben in northwest Jianghan Basin, the deformation characteristics are analyzed in detail and the stress field sequences are rebuilt. According to the deformation characteristics and the stress field sequences, combined with the evolution of regional tectonic and superimposed deformation features in this area, and the evolution history of the grabens in Jianghan Basin can be divided into four main stages: 1) Late Cretaceous to Paleogence, dominated by NEE-SWW-trending extension, the grabens formed in Jianghan Basin; 2) late Paleogence, the grabens deformed strongly by the E-W-striking tectonic compression; 3) Neogene, controlled by NE-SW-trending extension and NW-SE-striking extension in turn, the grabens were extended again; 4) late Neogene, dextral-slip activation occurred to the grabens due to NE-SW-striking compression. This study will be beneficial to research on tectonic evolution and the storage and migration of oil and gas in Jianghan Basin.

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田蜜,施炜,李建华,渠洪杰.2010.江汉盆地西北部断陷带构造变形分析与古应力场演化序列[J].地质学报,84(2):159-170.
tianmi, shiwei, lijianhua, quhongjie.2010. Tectonic Deformation Analysis and Paleostress Field Sequence of the Grabens[J]. Acta Geologica Sinica,84(2):159-170.

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  • 收稿日期:2009-07-10
  • 最后修改日期:2009-08-25
  • 录用日期:2009-08-31
  • 在线发布日期: 2010-01-08
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