西湖凹陷西部斜坡带平湖组源-汇体系特征
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摘要
西部斜坡带是东海陆架盆地西湖凹陷重要的油气勘探开发区域之一,寻找富砂区、明确砂体展布主控因素是油气勘探开发深入的关键。从源-汇体系研究出发,结合构造演化特征,总结了西部斜坡带平湖组物源体系、输砂体系及汇聚体系特征。研究结果表明,西部斜坡带具有海礁隆起及渔山东低隆起两大物源体系,下切沟谷输砂及坡折带控砂是主要的源-汇体系类型。构造特征差异控制了不同斜坡的源-汇模式:北部杭州斜坡发育沟谷加边界断裂坡折源-汇模式,中部平湖斜坡发育沟谷加断阶坡折源-汇模式,南部天台斜坡发育沟谷加挠曲坡折源-汇模式。杭州斜坡和平湖斜坡源-汇模式适合形成富砂区,转换带类型多样有利于形成构造控制下的岩性圈闭。
The west slope belt is one of the important oil and gas exploration and development areas in Xihu sag of East China Sea Shelf basin. The key of oil/gas exploration and development is to find rich sand area and figure out the main controlling factors of sand body distribution. Based on the study of Source-to-Sink system and the characteristics of tectonic evolution, this paper summarizes the provenance, sand-transporting and accumulating system of Pinghu Formation of west slope belt. The results show that the west slope has two major sources which are Haijiao uplift and Yushandong low uplift. Sand supply from incised valley and sand controlling of slope-break belt are main Source-to-Sink system types. The difference of structural characteristics controls Source-to-Sink systems of different slopes: The gully valley and boundary fault slope-break systems are developed in the northern Hangzhou slope; the gully valley and fault-step slope-break are developed in the central Pinghu slope; the gully valley and flexural slope systems are developed in the southern Tiantai slope. It is concluded that the Source-to-Sink systems in Hangzhou slope and Pinghu slope are favorable for the formation of rich sand area, and the variety of transition zones is beneficial to form lithologic traps under structural controls.
The west slope belt is one of the important oil and gas exploration and development areas in Xihu sag of East China Sea Shelf basin. The key of oil/gas exploration and development is to find rich sand area and figure out the main controlling factors of sand body distribution. Based on the study of Source-to-Sink system and the characteristics of tectonic evolution, this paper summarizes the provenance, sand-transporting and accumulating system of Pinghu Formation of west slope belt. The results show that the west slope has two major sources which are Haijiao uplift and Yushandong low uplift. Sand supply from incised valley and sand controlling of slope-break belt are main Source-to-Sink system types. The difference of structural characteristics controls Source-to-Sink systems of different slopes: The gully valley and boundary fault slope-break systems are developed in the northern Hangzhou slope; the gully valley and fault-step slope-break are developed in the central Pinghu slope; the gully valley and flexural slope systems are developed in the southern Tiantai slope. It is concluded that the Source-to-Sink systems in Hangzhou slope and Pinghu slope are favorable for the formation of rich sand area, and the variety of transition zones is beneficial to form lithologic traps under structural controls.
引文
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