1) Wumishan Formation
雾迷山组
1.
Study on Evolution Feature of Oilfield Water Quality in Renqiu Wumishan Formation;
任丘雾迷山组油藏开发过程中水质演化特征
2.
Microdigital stromatolites and their response to stromatolite decline at 1250Ma± for the Mesoproterozoic Wumishan Formation at Jixian section in Tianjin;
天津蓟县中元古界雾迷山组微指状叠层石及其对1250Ma±叠层石衰减事件的响应
3.
Stromatolite deposition and depositional environment in Wumishan formation of West Liaoning;
辽西凌源雾迷山组叠层石沉积特征及沉积环境分析
2) Dolomite of Wumishan Formation
雾迷山组白云岩
3) geothermal reservoir of the Jixian system
雾迷山组热储
1.
Wumishan geothermal reservoir of the Jixian system widely distributes in Tianjin and is the most important reservoir of geothermal development and utilization.
蓟县系雾迷山组热储层是天津地区分布最广、开发利用最重要的热储层。
4) the Wumishan Group of the Jixian System
蓟县系雾迷山组
1.
The results show that the Babaoshan fault is characterized by multi-activity from a reverse fault to a normal fault and the geothermal reservoir consisting of dolomite of the Wumishan Group of the Jixian System is a nose-type-anticline uplift.
结果表明,八宝山断裂的性质具有先逆断层后正断层的多期活动性特征;研究区蓟县系雾迷山组白云岩为鼻状背斜凸起型热储构造;深部热流主要沿着黄庄—高丽营断裂的上盘向上传导聚集;浅部古生界碳酸盐岩地层富集强径流冷地下水的作用使青白口系的地温梯度高于北京平原区,纵向地温场坡度较北京平原区大;临近深大断裂构造带导致地下热水具有放射性镭含量高的特征;地下热水的14C年龄特征反映城区地热田接受西部隆起区地下水的补给很少;地热井水头分布趋势反映雾迷山组白云岩热储地下热水受黄庄—高丽营断裂阻隔后由南向北方向径流。
5) Mesoproterozoic Wumishan Formation
中元古界雾迷山组
1.
Seismic-tsunami sequence and its geological features of Mesoproterozoic Wumishan Formation in Fangshan Global Geopark,Beijing,China:a case study on Yesanpo scenic dis-trict
北京房山世界地质公园中元古界雾迷山组地震-海啸序列及地质特征——以野三坡园区为例
2.
Seismically collapsed megabreccias(seismites)have been found in the lower part of the Second Member of the Mesoproterozoic Wumishan Formation(1.
在河北省涞源县白石山构造峰林游览路线上,中元古界雾迷山组(距今10～14亿年间)第二段地层下部,发现“震动坍塌巨角砾岩”(震积岩)。
6) Wumishan cyclothems
雾迷山旋回层
补充资料：转迷开悟
【转迷开悟】
（术语）舍三界生死之迷，达于涅槃之悟也。离烦恼之迷，得菩提之证也。
（术语）舍三界生死之迷，达于涅槃之悟也。离烦恼之迷，得菩提之证也。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条