惠州凹陷断裂几何学特征及成因机制

    Geometrical characteristics and genesis mechanism of Huizhou Sag rupture

    • 摘要: 惠州凹陷作为珠江口盆地珠一坳陷带内重要的富烃凹陷,其断裂系统的几何学特征及成因机制对油气勘探开发具有关键意义。本文基于高精度三维地震资料与地震测线解析,在前人研究的基础上,结合区域构造演化背景,系统分析了惠州凹陷不同级别断裂的平面及剖面几何特征,并探讨了不同走向断裂的成因差异及它们对油气成藏的影响。研究表明:(1)研究区断裂以伸展正断层为主,可大体分为3个级别。剖面上,一级断裂以高角度铲式、板式及坡坪式为典型,二、三级断裂多为直立板式,组合样式多出现Y形、多米诺式、X形、人字形、入字形等。(2)平面上,一级断裂走向有NE、NW、近EW向,呈右旋斜列式展布;二级断裂走向以NW向为主,三级断裂走向以NW、近EW向为主,呈雁列式展布。(3)断裂系统受控于基底断裂继承性与多期应力场叠加。燕山期NE—SW向基底断裂活化形成NE和NW向断裂;裂陷晚期应力场旋转诱发近EW向断裂发育;构造活化期断裂叠加右旋走滑改造。(4)NE向断裂主导早期垂向运移,EW向断裂驱动晚期成藏,NW向断裂调节圈闭形成。研究成果揭示了多期构造活动对断裂几何特征的控制机理,为未来惠州凹陷油气资源勘探开发提供科学依据。

       

      Abstract: As an important hydrocarbon-rich depression in the Zhuyi Depression of the Pearl River Estuary Basin, the geometric features and genesis mechanism of the Huizhou sag are of key significance for hydrocarbon exploration and development. Based on high-precision 3D seismic data and seismic line analysis, this paper systematically analyses the planar and sectional geometric features of different levels of fractures in the Huizhou Sag on the basis of previous studies and in the context of the tectonic evolution of the region, and explores the differences in the genesis of fractures with different orientations, and their impact on oil and gas formation and reservoirs. The study shows that: (1) the fractures in the study area are mainly extensional normal faults, which can be roughly divided into three levels. In profile, the first grade fractures are typical of high-angle shovel-type, plate-type and slope-ping-type, while the second and third grade fractures are mostly upright plate-type, and the combination styles are Y-shaped, domino-type, X-shaped, herringbone, and zig-zag. (2) On the plane, the first level of fractures are orientated towards NE, NW and near EW, spreading in a right-handed diagonal column; the second level of fractures are mainly orientated towards NW, and the third level of fractures are mainly orientated towards NW and near EW, spreading in a geese column. (3) The fracture system is controlled by the succession of basement fractures and the superposition of multi-period stress field. During the Yanshan period, the NE-SW oriented basement fractures were activated to form NE and NW oriented fractures; during the late rift period, the rotation of the stress field induced the development of near EW oriented fractures; and during the tectonic activation period, the fractures were superimposed on the dextral strike-slip modification. (4) NE-directed fractures dominated the early vertical transport, EW-directed fractures drove the late reservoir formation, and NW-directed fractures regulated the trap formation. The research results reveal the control mechanism of multi-phase tectonic activities on the geometric features of fractures, which will provide scientific basis for the future exploration and development of oil and gas resources in Huizhou Sag.

       

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