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Accumulation conditions and exploration directions of natural gas in deep subsalt Sinian-Cambrian System in the eastern Sichuan Basin, SW China

机译:中国四川盆地东部深盐下震旦-寒武系天然气成藏条件和勘探方向

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Based on comprehensive analysis of outcrops and drilling data, and interpretation of more than 6×104km2seismic data, this paper delineates the regional distribution of the gypsum-salt layers in Middle-Lower Cambrian in eastern Sichuan Basin, and discusses accumulation conditions for natural gas in deep subsalt Sinian-Cambrian System in eastern Sichuan Basin, and points out favorable exploration directions. There are two sets of regional gypsum-salt layers in the Middle-Lower Cambrian in eastern Sichuan Basin, which are regional detachment layers, with fault-related folds occurring above and broad anticlines occurring below. There are 6-7 rows of NNE and NE trending large traps developed under the salt. Good space configuration of source rocks, reservoirs and cap rocks provide favorable accumulation conditions for natural gas in the deep subsalt in this region: three sets of hydrocarbon source rocks including Sinian Doushantuo Formation, the third Member of Sinian Dengying Formation, and dominant Cambrian Shuijingtuo Formation; three sets of weathering crust karst reservoirs and grain beach reservoirs including the second and fourth Members of Sinian Dengying Formation, and Cambrian Shilongdong Formation; and the regional cap of gypsum-salt in the Middle-Lower Cambrian and shale in Shuijingtuo Formation. The top target in deep subsalt exploration in eastern Sichuan Basin should be the fourth Member of Dengying Formation, followed by Shilongdong Formation and the second Member of Dengying Formation, and areas on migration direction with appropriate burial depth and being far away from the edge of the basin should be the first choices in exploration. Therefore, the favorable hydrocarbon exploration areas in the near future are the Honghuadian-North Huaying Mountain, Liangshuijing-Pubao Mountain-Leiyinpu, and Datianchi structural belts.
机译:在对露头和钻探资料进行综合分析,并对6×104 km2以上地震资料进行解释的基础上,描述了川东中下寒武统石膏盐层的区域分布,并探讨了四川盆地天然气的成藏条件。川东地区深层盐下震旦-寒武系,并指出了有利的勘探方向。四川盆地东部中下寒武统有两套区域性石膏盐层,即区域性脱离层,断层相关褶皱发生在上层,背斜发育在下部。在盐下形成了6-7行NNE和NE趋势大的圈闭。烃源岩,储集层和盖层的良好空间构造为该地区深层盐下的天然气提供了有利的聚集条件:震旦系斗山ush组,震旦系灯影组第三段和寒武纪水井ing组等三套烃源岩。 ;震旦系灯影组第二,第四段,寒武纪石龙洞组三组风化壳岩溶储集层和粮滩储集层;以及水井tu组中下寒武统和页岩的石膏盐区域盖。四川盆地东部深层盐下勘探的最高目标应该是灯影组的第四段,其次是石龙洞组和灯影组的第二段,并且在适当的埋藏深度且远离岩心边缘的迁移方向区域。盆地应该是勘探的首选。因此,在不久的将来,有利的油气勘探地区是:红花店—北华鹰山,凉水井—普宝山—雷音普和大田池构造带。

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