塔中地区上奥陶统礁滩复合体储层地震预测技术
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摘要
塔中Ⅰ号坡折带位于塔中古隆起北斜坡大型碳酸盐岩台地北缘,呈北西-南东走向,台缘坡折带长220 km,宽8~18 km,发育上奥陶统大型礁滩复合体,油气藏埋深3 700~7 200 m。该带地表沙丘起伏,地下结构复杂,地震剖面品质差,奥陶系碳酸盐岩储层埋深大,非均质性强,储层控制因素复杂。通过地质、测井、岩心和试油等资料分析了奥陶系礁滩体不同类型储层的地球物理响应特征,总结出适合于该带碳酸盐岩礁滩体储层预测的方法,对上奥陶统礁滩复合体发育分布规律进行了精细描述,在礁滩体复合体的勘探中取得了很好的勘探成果。
Tazhong-Ⅰ slopebreak zone is located at the north margin of the large carbonate platform developed on the northern slope of Tazhong paleo-uplift.The northwest trending slope break is 220 km long and 8-18 km wide.It developed large reef-flat complexes in the Upper Ordovician and harbors giant condensate gas reservoirs with burial depth of 3 700-7 200 m.High-quality seismic profiles are hard to acquire here because of the undulate dunes at the surface and complex structures underground.And the accuracy of lateral reservoir prediction is low due to the deep burial depth of the Ordovician carbonate reservoirs,high heterogenity,and multiple controlling factors upon reservoir development.However,a set of methods have been developed and applied successfully to the prediction of the reef-flat carbonate reservoirs through analyzing geophysical responses to various types of Ordovician reef-shoal complex reservoirs based on geologic log,core,and test data.The application of these methods has accelerated the exploration of large condensate gas reservoirs in the slope break zone.
Tazhong-Ⅰ slopebreak zone is located at the north margin of the large carbonate platform developed on the northern slope of Tazhong paleo-uplift.The northwest trending slope break is 220 km long and 8-18 km wide.It developed large reef-flat complexes in the Upper Ordovician and harbors giant condensate gas reservoirs with burial depth of 3 700-7 200 m.High-quality seismic profiles are hard to acquire here because of the undulate dunes at the surface and complex structures underground.And the accuracy of lateral reservoir prediction is low due to the deep burial depth of the Ordovician carbonate reservoirs,high heterogenity,and multiple controlling factors upon reservoir development.However,a set of methods have been developed and applied successfully to the prediction of the reef-flat carbonate reservoirs through analyzing geophysical responses to various types of Ordovician reef-shoal complex reservoirs based on geologic log,core,and test data.The application of these methods has accelerated the exploration of large condensate gas reservoirs in the slope break zone.
引文
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12邬光辉,李启明,张宝收,等.塔中Ⅰ号断裂坡折带构造特征及勘探领域[J].石油学报,2005,1(1):27~37
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2苗继军,贾承造,邹才能,等.塔中地区下奥陶统岩溶风化壳储层特征与勘探领域[J].天然气地球科学,2007,18(4):497~500
3韩革华,漆立新,李宗杰,等.塔河油田奥陶系碳酸盐岩缝洞型储层预测技术[J].石油与天然气地质,2006,27(6):860~870
4殷积峰,李军,谢芬,等.川东二叠系生物礁油气藏的地震勘探技术[J].石油地球物理勘探,2007,42(1):70~75
5陈学强,段孟川,钟海,等.塔中沙漠区碳酸盐岩三维地震勘探技术[J].勘探地球物理进展,2006,29(5):346~352
6鲍祥生,尹成,赵伟,等.储层预测的地震属性优选技术研究[J].石油物探,2006,45(1):28~33
7佘德平,曹辉,郭全仕.断裂系统解释与储层预测中的三维相干技术[J].石油与天然气地质,2007,28(1):100~105
8李明娟,张永贵,邬兴威,等.塔河南部地区碳酸盐岩油气预测技术研究[J].石油与天然气地质2006,27(4):536~541
9王者顺,王尚旭,唐文榜.塔河碳酸盐岩溶洞油藏的地震响应及频率差异分析[J].石油与天然气地质,2004,25(1):93~101
10毕研斌,龙胜祥,郭彤楼,等.应用频率衰减属性预测TNB地区储层含气性[J].石油与天然气地质,2007,28(1):116~120
11杨海军,邬光辉,韩剑发,等.塔里木盆地中央隆起带奥陶系碳酸盐岩台缘带油气富集特征[J].石油学报,2007,28(4):27~29
12邬光辉,李启明,张宝收,等.塔中Ⅰ号断裂坡折带构造特征及勘探领域[J].石油学报,2005,1(1):27~37
13顾家裕,张兴阳,罗平,等.塔里木盆地奥陶系台地边缘生物礁、滩发育特征[J].石油与天然气地质,2005,26(3):277~283
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