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首页> 外文期刊>Marine and Petroleum Geology >Present-day stress and pore pressure fields in the Cuu Long and Nam Con Son Basins,offshore Vietnam
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Present-day stress and pore pressure fields in the Cuu Long and Nam Con Son Basins,offshore Vietnam

机译:越南近海Cuu Long和Nam Con Son盆地现今的应力和孔隙压力场

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摘要

Knowledge of the in situ,or contemporary stress field is vital for planning optimum orientations of deviated and horizontal wells,reservoir characterization and a better understanding of geodynamic processes and their effects on basin evolution.This study provides the first documented analysis of in situ stress and pore pressure fields in the sedimentary formations of the Cuu Long and Nam Con Son Basins,offshore Vietnam,based on data from petroleum exploration and production wells.In the Cuu Long Basin,the maximum horizontal stress is mainly oriented in NNW-SSE to N-S in the northern part and central high.In the Nam Con Son Basin,the maximum horizontal stress is mainly oriented in NE-SW in the northern part and to N-S in the central part of the basin.The magnitude of the vertical stress has a gradient of approximately 22.2MPa/km at 3500 m depth.Minimum horizontal stress magnitude is approximately 61% of the vertical stress magnitude in normally pressured sequences.The effect of pore pressure change on horizontal stress magnitudes was estimated from pore pressure and fracture tests data in depleted zone caused by fluid production,and an average pore pressure-stress coupling ratio(DELTA S_h/DELTA P_p)obtained was 0.66.The minimum horizontal stress magnitude approaches the vertical stress magnitude in overpressured zones of the Nam Con Son Basin,suggesting that an isotropic or strike-slip faulting stress regime may exist in the deeper overpressured sequences.
机译:对原位或当代应力场的了解对于规划斜井和水平井的最佳方位,储层特征以及更好地理解地球动力学过程及其对盆地演化的影响至关重要。根据石油勘探和生产井的数据,在越南近海的Cuu Long和Nam Con Son盆地的沉积地层中形成孔隙压力场。在Cuu Long盆地,最大水平应力主要集中在NNW-SSE到NS在南康松盆地中,最大水平应力主要集中在北部的NE-SW和盆地中部的NS。垂直应力的大小为在3500 m深度时约为22.2 MPa / km。在正常压力序列中,最小水平应力幅值约为垂直应力幅值的61%。根据产液引起的衰竭区的孔隙压力和裂缝测试数据,估算了水平应力幅值的确定变化,平均孔隙压力-应力耦合比(DELTA S_h / DELTA P_p)为0.66。 Nam Con Son盆地超压带的垂直应力幅值,这表明在较深的超压层序中可能存在各向同性或走滑断层的应力状态。

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