摘要
珠江口盆地白云凹陷作为我国深水勘探研究的重要战略目标区之一,该区域中新统珠江组广泛存在的抱球虫灰岩主要为含泥、粉砂质抱球虫灰岩和抱球虫粉砂质泥质灰岩两类,前者具有较高的孔隙度和储集性,为一类潜在深水相储集层,后者原生孔隙保存较差,不太有利于储层发育。珠江组抱球虫灰岩后生成岩作用以机械压实作用为主,压溶作用为辅。
The Baiyun Sag of Pearl River Mouth Basin is one of the key strategic goals in the deep-water exploration in China. The globigerinid limestone deposits, which are widely existed in the Miocene Zhujiang Formation, are Mainly divided into silt, silt with the ball of coccidia and clover-bearing gravel muddy limestone. The former has high porosity and reservoir property, and is a kind of potential deep water reservoir. While there is poorly preserved and is not conducive to reservoir development in the latter porosity. The post-diagenesis of the pelagic limestone in Zhujiang Formation is mainly mechanical compaction, and the pressure solution is secondary.
出处
《世界有色金属》
2016年第12期175-175,177,共2页
World Nonferrous Metals
关键词
珠江口盆地
白云凹陷
珠江组
抱球虫灰岩
机械压实作用
Pearl River Mouth Basin
The Baiyun Sag
Zhujiang Formation
globigerinid limestone
mechanical compaction