孟加拉湾若开海域晚新生代构造变形及其对油气的控制作用

作    者:唐鹏程1,邵大力1,王海强2,王红平1,孙 辉1,张勇刚1,马宏霞1,丁梁波1
单    位:(1 中国石油杭州地质研究院;2 中油国际(凯尔)有限责任公司)
基金项目:受中国石油天然气集团公司科学研究与技术开发项目“海外重点战略大区勘探技术研究与实践”子课题资助
摘    要:
利用钻井、二维和三维地震资料,剖析了孟加拉湾若开海域晚新生代的构造变形特征,探讨了构造变形对油气的控制作用。区域深度地质剖面揭示,研究区南部仅发育底部滑脱层(深度10 km),而北部则发育底部滑脱层(深度12 km)和中部滑脱层(深度4 km);受滑脱层的控制,研究区南部仅发育一套构造层,而北部则发育变形不协调的上、下两套构造层;南部背斜的南北向延伸距离、波长及背斜间隔距离均明显大于北部。通过北部局部构造精细解析表明,研究区北部变形相对较复杂,上构造层主要发育近南北向的背斜和次级张扭性右旋走滑断层,二者形成时间分别为晚第四纪和晚第四纪末。若开海域晚新生代的构造变形对圈闭形成、油气运聚和保存条件具有重要的控制作用。指出研究区南部平缓褶皱带构造—岩性复合圈闭具备形成大油气田的条件,是下一步油气勘探的重要目标。
关键词:孟加拉湾;若开褶皱带;晚新生代;构造特征;油气聚集

Late Cenozoic Deformation of Arakan Fold Belt and Its Control on Hydrocarbon Accumulation in Offshore Rahkine, Bay of Bengal

Author's Name: Tang Pengcheng,Shao Dali, Wang Haiqiang, Wang Hongping, Sun Hui, Zhang Yonggang, Ma Hongxia, Ding Liangbo
Institution: PetroChina Hangzhou Institute of Geology
Abstract:
Based on recent drilling and 2D/3D seismic data, the late Cenozoic deformation of Arakan fold belt and its control on hydrocarbon accumulation was investigated in offshore Rahkine, Bay of Bengal. The analysis result shows that only a basal detachment fault (10km of burial depth) develops in the southern part of the study area while a basal detachment fault (12km deep buried) and a middle detachment fault (4km deep) develop in the northern part. Under the control of these detachment faults, one set of tectonic layers develops in the southern part and two sets of layers (the upper and the lower one) in the northern part, respectively. The lateral extended distance, the wave length and the interval distance between anticlines are longer obviously in the southern part than those in the northern part. In addition, both the NS-trending anticline and the secondary NE-trending transtensional dextral strike-slip fault formed in the upper tectonic layer in northern part. According to growth strata records, these deformations formed in late Quaternary and at the end of late Quaternary respectively. Trap formation, hydrocarbon migration and accumulation conditions are greatly controlled by the late Cenozoic deformation. It is suggested that the structural-lithologic composite traps have the condition to form large gas fields in the gentle fold belt and the southern part of the study area is the favorable exploration targets in the future.
Keywords: Late Cenozoic; Structural characteristics; Hydrocarbon accumulation; Arakan fold belt; Bay of Bengal
投稿时间: 2015-01-12  
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