摘要
综合利用泥岩声波时差法、镜质组反射率（Ro）法和地层对比法对Bongor盆地中生界剥蚀厚度进行了恢复，恢复结果表明Bongor盆地中生界的剥蚀厚度在1000--2000m之间，呈现出南北大、中间小的特征。快速而剧烈的抬升剥蚀使得该盆地下成藏组合P组砂体的储集能力得以保存;反转期的挤压应力导致了盆地地层的褶皱变形，形成了一系列断背斜、断鼻构造，为油气成藏提供了良好的圈闭条件；反转引起的断层活化为Bongor盆地中油气的运移提供了通道。
Mesozoic erosion thickness of Bongor Basin was restored using mudstone acoustic time difference method, vitrinite reflectance （Ro） method, and stratigraphic correlation method. Result showed that the erosion thickness ranged from 1000 to 2000 m, thick in northern and southern slope while thin in central sag. The quick but intense uplift preserved the good reservoir quality of the P Formation sand body in the lower play. The compressive stress during inversion folded the strata and contributed to the formation of a lot of faulted anticlines and noses which were excellent traps for hydrocarbon accumulation. The fault reactivation triggered by inversion promoted the hydrocarbon migration in Bongor Basin.
出处
《中国石油勘探》
CAS
2013年第5期45-53,共9页
China Petroleum Exploration
基金
国家重大科技专项"中西非裂谷系综合评价及勘探技术"(2011ZX05029-001)
中国石油勘探开发研究院项目"中非裂谷系反转裂谷盆地构造样式及成藏模式研究"(2012Y-056)
关键词
反转盆地
剥蚀厚度
油气聚集
Bongor盆地
乍得
inverted basin, erosion thickness, hydrocarbon accumulation, Bongor Basin, Chad
