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The Distribution Controlling Factors of Reef and Shoal, and Their Favorabl e Plays Analysis: Changxing(Permian)- Feixianguan Formations(Triassic), Sichuan Basin

机译:珊瑚礁和浅滩的分布控制因素及其最有利的e播放分析:长兴(二叠纪) - 四川盆地(三叠纪)

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Reef and shoal gas reservoirs in the Permian-Triassic Changxing-Feixianguan formations, Sichuan Basin, are typical represent ative of the marine carbonatite gas reservoirs in china. Breakthroughs in exploration make it necessary to know the distribution controlling factors of reef and shoal. Based on the comparative analysis of various well data and 3D seismic, the impact of var ious factors is studied on the distribution of reef and oolitic shoal, such as the geometry of the Kaijiang-Liangping trough, Late Permian regional palaeogeomorphologic framework, tectonic extension, system tracts of the Longtan-Feixianguan formations. The following conclusions were drawn. (1) At the end of Late Permian, the palaeogeomorphologic framework of the Sichuan Basin was "three depressions separated by three uplifts" which played a key role in controlling the distribution of reefs and ool itic shoals. (2) Transgressive systems tract (TST) deposits dominated the Longtan-early Changxing period , mid-late Changxin g period has a highstand system tract (HST) deposits feature. Highstand system tract (HST) deposits dominated Feixianguan p eriod. The change of system tracts made it possible to develop multistage reefs near the platform margin. Oolitic shoals may o ccur on the progradation slope margin in the Kaijiang-Liangping trough, while the aggradational platform margin is the most f avorable development zone of Oolitic shoals. (3)The unevenness of extension caused the differences in the development of platform margin palaeogeomorphologic, which influenced the development time, continuity and their superimposed relationsh ip of reef and oolitic shoal. (4)The methods, based on 3D seismic, are studied for characterizing the bioherms distribution a long the platform margin. The distribution and shape of Bioherms along the platform margin can occur as curved belt, monilif orm and atoll, or occur as echelon belt oblique to the platform margin. Favorable Plays are analyzed based on the study results.
机译:四川盆地二叠纪 - 三叠纪常兴 - 飞翔园区礁石和浅滩煤气藏是典型的代表中国海洋碳酸盐石储气储层。勘探中的突破使得有必要了解珊瑚礁和浅滩的分布控制因素。基于各种井数据和3D地震的比较分析,研究了疣的影响对礁石和鲕粒浅滩的分布,如凯江 - 梁平槽的几何形状,后期二叠纪古神经形式框架,构造延伸,龙潭 - 飞翔组织的系统。提出了以下结论。 (1)在二叠纪后期,四川盆地的古代正像艺术框架是“三个隆起分开的三个萧条”在控制珊瑚礁和OOL Itic Shoals的分布方面发挥了关键作用。 (2)近期船舶(TST)沉积物主导龙潭 - 早期的长兴时期,中期长兴克期间有一个高价系统的沉积物(HST)沉积功能。高层系统道(HST)沉积物主导菲建源P eriod。系统束的变化使得可以在平台边缘附近开发多级珊瑚礁。 oolitic shoals可以在开江 - 梁平槽中的促成坡度缘,而加重平台边缘是欧隆浅滩中最不可移动的开发区。 (3)延伸不均匀导致平台边距开发的差异,影响了礁石和鲕粒的开发时间,连续性和叠加关系。 (4)研究了基于3D地震的方法,用于表征生物学分布长平台边距。沿着平台边缘的生物的分布和形状可以作为弯曲带,单色矿石和环礁,或者发生在平台边距的梯队带倾斜。基于研究结果分析有利的戏。

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