贵州松桃杨家湾-黑水溪南华纪早期成锰盆地特征及深部锰矿找矿预测  

Characteristics of Early Manganese Formation Basin in Songtao Yangjiawan-Heishui River,Guizhou Province and Prospecting of Deep Manganese Ore

作　　者：蒋天锐[1] 杨胜堂[1] 袁良军[1] 谢兴友[1] Jiang Tianrui;Yang Shengtang;Yuan Liangjun;Xie Xingyou(Geological Brigade 103,bureau of Geology and mineral resxources,Guizhou Province,Guizhou Tongren 554300)

机构地区：[1]贵州省地矿局103地质大队,贵州铜仁554300

出　　处：《云南化工》2020年第9期98-100,共3页Yunnan Chemical Technology

基　　金：贵州省地质矿产勘查开发局地质科研项目《贵州松桃杨家湾—黑水溪地区深部锰矿找矿预测研究》(合同编号:黔地矿科合(2016)06号)时间:2016.12-2020.12。

摘　　要：通过对杨家湾-黑水溪南华纪早期成锰盆地的研究和原形结构特征恢复,杨家湾-黑水溪大型锰矿床乃属同一IV级地堑成锰盆地。目前该盆地已控制形成了杨家湾大型锰矿床、黑水溪小型锰矿床、三角坡小型锰矿床等古天然气渗漏沉积型锰矿床,预测深、边部仍具较大的找矿潜力。Through the study of the early South China manganese basin of Yangjiawan heishuixi and the restoration of its original structural characteristics,the Yangjiawan heishuixi large manganese deposit belongs to the same IV grade graben manganese basin. At present,the basin has controlled the formation of Yangjiawan large manganese deposit,heishuixi small manganese deposit,triangle slope small manganese deposit and other paleo natural gas leakage sedimentary manganese deposits. It is predicted that there is still great prospecting potential in the deep and edge areas.

关 键 词：成锰盆地 沉积特征 找矿预测 贵州松桃 

分 类 号：P618.32[天文地球—矿床学]