综合地震解释、二维建模以及岩石物理和地震属性分析来破译巴基斯坦Missakeswal地区的油气潜力

A. Abbas, Hongtao Zhu, A. Anees, U. Ashraf, N. Akhtar
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引用次数: 19

摘要

Missakeswal是一个重要的油气田,位于青藏高原喜马拉雅造山带活动前陆褶皱和冲断带上。二维地震数据(SEG-Y、导航和地震速度)和测井数据的综合研究有助于我们圈定该地区潜在的储层岩石。基于地层研究和井顶的地震解释有助于标记四个反射面;乔加里,萨克萨,洛哈特和地下室。利用速度分析系统将时间剖面转换为深度剖面,圈定地下构造。此外,深层剖面断界背斜和地壳缩短分析表明,早于逆断裂和盆地构造的沉积序列褶皱有利于油气成藏。解释地震剖面的二维建模证实了沉积序列中的逆断层和基底中的正断层。此外,进行了地震属性分析,有助于了解横向连续性、层序和期望层厚度,突出了含油气系统,并肯定了解释结果。识别出的构造变化有助于认识区域构造环境,同时也有助于了解储层在横向厚度变化、断层偏移和岩性差异方面的特征。揭示了Sakesar组和Chorgali组碳酸盐岩层序是Missakeswal地区潜在的储集层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Integrated Seismic Interpretation, 2D Modeling along with Petrophysical and Seismic Attribute Analysis to Decipher the Hydrocarbon Potential of Missakeswal Area, Pakistan
Missakeswal is an important hydrocarbon field, lying on active foreland fold and thrust belt of Himalayan orogeny in Potwar plateau. Integrated study of 2D seismic data (SEG-Y, Navigation and seismic velocities) and well logs helps us to delineate the potential reservoir rock of the area. Seismic interpretation based on stratigraphic studies and well tops, aids to mark four reflectors; Chorgali, Sakesar, Lockhart and Basement. Time sections are converted to depth section using velocity analysis system to delineate subsurface structure. Besides this, fault-bounded anticlines and crustal shortening analysis of the depth sections, revealed that folding in the sedimentary successions pre-date reverse faulting and regime of the Potwar basin, is suitable for hydrocarbon accumulation. 2D modeling of the interpreted seismic sections confirms reverse faulting in the sedimentary successions and normal faulting in the basement. Moreover, Seismic Attributes Analysis has carried out which helps in understanding the lateral continuity, bedding sequences and thickness of desired beds highlighted the petroleum system and affirmed the interpretation. The identified structural variations would help in the understanding of the regional tectonic settings, besides this, reservoir character in terms of lateral thickness variation, fault offsets and lithological dissimilarities are achieved. It also reveals that carbonate successions of the Sakesar and Chorgali formations acted as potential reservoirs in Missakeswal area.
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