据此得出北京地区雾迷山组碳酸盐湖汐沉积模式。
Therefore, a tidal sediment model for carbonatite of the Wumi - shah Formation in Beijing area can be drawn out.
本文进一步提出了蓟县地区中元古界雾迷山组中存在着风暴沉积的证据。
This paper, however, presents evidence of the presence of storm deposits in the middle Proterozoic Wumishan Formation in the Jixian area.
公乐亭泉出露于蓟县系雾迷山组白云岩地层与第四地层接触部位，为溢出泉。
Gongleting spring emerges at the contact place between the dolomite of wumishan formation, jin system and the stratum of quaternary system and is an overflow spring.
雾迷山组（Wumishan Fm）曾称雾迷山灰岩。位于蓟县系中下部，分布于冀北一带。为一套富镁的巨厚碳酸盐建造，韵律明显，以含有各种燧石结核和条带状白云质灰岩为主,夹纯灰岩、白云岩、绿色砂页岩等。含叠层石Pseudogymnosolen mopanyuensis、Scyphus parvus、Conophyton lituum；微古植物化石有Asperatopsophosphaera umishanensis、A.umishanensis var.minor等。厚3340米。与下伏杨庄组为连续沉积。底部在河北西北部有铁矿层。雾迷山组沉积期古地磁极性为负极性，古磁极位置-18 2°N，49 2°。
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