河北承德大庙黑山铁矿床位于大庙斜长岩体南部边缘，红石砬—大庙深断裂附近北侧。
The Damiao iron deposit is located at the southern margin of the Damiao plagioclase rock body and northern side of the southern edge of Hongshila-Damiao deep fault.
这类矿床多分布在地台稳定区的边缘，常沿深断裂或裂谷带延展方向呈群分布。
They are commonly distributed along the margins of such stable areas as the platform and are characterized by oriented distribution along extensions of deep faults or rifts.
二级成矿边缘为区域深大断裂边缘，控制区域成矿带形成；
The first ore-forming margin is the interface where Huabei plate and Yangzi plate(two sides of Shanyang to Xixia faulted zone), which control the forming of two major mineralization belt;
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