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补作勘探区位于水公河向斜东翼,整体为向水公河倾斜的近“S”的单斜构造。煤岩层走向近南北向,倾向近东西向。在区域构造的控制下,经后期的燕山运动的改造,区内次一级构造形迹分布规律很明显。北部主要受东西向黔中断裂的控制;西部主要受东西向黔中断裂和南西向水城-紫云断裂的控制;东部主要受贵阳-师宗断裂构造的控制;南部主要受水城-紫云断裂和贵阳-师宗断裂构造的控制。
The Buzuo prospecting area is located in the east of the Shuigonghe syncline and is generally composed of a monoclinic structure near the “S ” inclined to the Shuigonghe River. The coal rock formation is nearly north-south direction and tends to be nearly east-west. Under the control of regional tectonics, through the transformation of Yanshan movement in the later period, the sub-primary tectonic distribution pattern in the area is obvious. The northern part is mainly controlled by the east-west-central Guizhou fault; the western part is mainly controlled by the east-west-central Guizhou fault and the southwest-wuxiang-Ziyun fault; the eastern part is mainly controlled by the Guiyang- Shizong fault structure; the southern part is mainly affected by the Watertown-Ziyun fault And Guiyang - Shizong fault structure control.