准噶尔盆地前哨地区有利砂体展布规律及演化模式——以下侏罗统三工河组二段一砂组为例
邱恩波 , 仇鹏 , 石磊 , 郭巧珍 , 雍建兴 , 闫利恒 , 兰浩
东北石油大学学报 ›› 2024, Vol. 48 ›› Issue (1) : 61 -73.
准噶尔盆地前哨地区有利砂体展布规律及演化模式——以下侏罗统三工河组二段一砂组为例
Distribution and evolution of favorable sand in Qianshao Area of Junggar Basin: a case study from the first sand group of the second member of the Sangonghe Formation of the Lower Jurassic
ed. Based on core observation, grain size analysis, logging and seismic data, combined with the principle of sequence stratigraphy, using phase conversion technology and seismic multi-attribute fusion technology, the favorable sand types, sand distribution regulation and evolution model are defined. The results show that the favorable sands in the study area are mainly underwater distributary channel in the inner front of shallow water delta, underwater distributary channel sand in the outer front of shallow water delta and sublacustrine fan sand caused by sandy debris flow. Along the source direction, the delta front sand controlled by the secondary slope break zone gradually transits to the sublacustrine fan sand under the third slope break zone. The favorable sand is the product of lake transgression stage, which is evolved from three retrogradation cycles. Controlled by multi-stage slope break zones, the first and second regression cycles form sublacustrine fan sand caused by sandy debris flow, and the third cycles form shallow water delta outer front sand and shallow water delta inner front sand. This study has guiding significance for the exploration and development target deployment of lithologic reservoirs in Sangonghe Formation in Qianshao Area.
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中国石油天然气集团公司新疆重大科技专项(2017E-0410)
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