intraformational conglomerate

Characteristics and genetic mechanism on structural conglomerate from Bayannuorigong area, Inner Mongolia;

内蒙古巴彦诺日公地区构造砾岩特征及其形成机制

Hycinth bean shaped tectonic mudstone conglomerate has been formed on the certain positions of the roof and the footwall in the quartz vein because of the late tectonic activity.

石英脉经过后期构造活动，顶底板一定位置形成扁豆体状构造泥砾岩，长期的氧化淋滤，石英脉中的金发生迁移，在构造泥砾岩中发生次生富集，形成金的富矿体。

The host rock is a tectonic breccia,the proximal enclosing rock is C phyllite.

近矿围岩为含碳千枚岩，赋矿岩石为构造角砾岩。