背斜圈闭是由于储集层发生褶皱变形(顶面向上拱起),其上部又为非渗透性岩层(盖层)所覆盖遮挡而形成,其内可以聚集石油和天然气的封闭地质构造。
圈闭类型主要为背斜圈闭及单斜圈闭。
火焰山构造带受基底逆冲断裂控制,断裂控制背斜圈闭形成。
Huoyanshan structure belts are controlled by the basement thrusts. The formation of anticline traps is controlled by the faults.
文章研究了背斜圈闭构造控制玉龙斑岩-矽卡岩型铜(钼)矿的形成和矿体的分布。
This paper studied the formation of the Yulong porphyry copper deposit controlled by the anticline trap structure and the distribution of the ore bodies.
应用推荐