“满银沟运动”系四川省地质局403队二分队和成都地质矿产研究所在四川会东满银沟矿区工作时,根据紫红色含铁岩系与下伏碳酸盐岩石的接触关系,于1970年确立和命名的;并据此将“不整合面”以上的含铁岩系划归力马河组第一段,下伏碳酸盐岩系仍归属通安组第四段。1973年成都所申玉莲对“满银沟运动”的地质特征作了论述。1975 “Full Silver Groove Movement” Department of Sichuan Geological Bureau 403 team second unit and the Chengdu Institute of Geology and Mineral Resources in Sichuan Huidong Man silver groove mine work, according to purple mafic rock series and underlying carbonate rock contact, Was established and named in 1970; accordingly, the iron-bearing rock series above the “unconformity” have been assigned to the first section of the Limahe Formation. The underlying carbonate series still belong to the fourth section of the Tong’an Formation. In 1973, he applied the “Geyingou Movement” geological characteristics in Chengdu. 1975