摘要
碳酸盐岩断裂带往往具有较宽阔的破碎带，是缝洞体储层发育的有利部位，断层破碎带的识别与预测对油气井位的优选具有重要意义。在塔里木盆地哈拉哈塘地区奥陶系碳酸盐岩井-震响应分析的基础上，通过地震方法与技术的对比分析，利用相干加强（AFE）与裂缝地震相分析技术，结合地震均方根振幅、地震曲率、缝洞体雕刻等多技术手段，可以进行碳酸盐岩断层破碎带的预测与刻画。结果表明，哈拉哈塘地区碳酸盐岩断层破碎带沿断裂带条带状、扇状展布，一般具有200-2500m的较宽范围，与钻探结果吻合程度高。哈拉哈塘地区奥陶系碳酸盐岩大型缝洞体储层的分布受控于断层破碎带，破碎带规模越大，缝洞体越发育。
Carbonate fault zone often has relatively wide damage zone,which is favorable for the development of fracture-cave system,and its identification and prediction is of great significance for oil/gas target optimization.On the basis of well-seismic responses analysis of the Ordovician carbonates in Halahatang area of the Tarim basin,comparative analysis of various seismic techniques reveals that the carbonate fault fractured zone can be identified and described by using coherent enhancement technique（AFE） and fracture seismic facies analysis technique,combining with the seismic root-mean-square amplitude,seismic curvature and fracture-cave system description.The results show that the carbonate fault damage zones are in stripped,fan-shaped distribution along the fault zone,generally with a width of 200-2500 m,which have good agreement with the well data.The fault fractured zone controlled the distribution of large scale fracture-cave system,and the wider the damage zone is,the larger the fracture-cave system is.
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
2016年第5期786-791,共6页
Oil & Gas Geology
基金
国家科技重大专项(2011ZX05004-004)
关键词
破碎带宽度
走滑断裂
碳酸盐岩
塔里木盆地
damage zone width, strike-slip fault, carbonate rock, Tarim Basin
