贵州地区下寒武统黑色岩系区“多元素”富集矿层分析及土壤重金属污染研究进展  

Research progress of polymetallic deposit and soil heavy metal pollution in Lower Cambrian black rock area in Guizhou

作　　者：王兴富[1] 顾秉谦 

机构地区：[1]贵州师范大学地理与环境科学学院,贵州贵阳550001

出　　处：《贵州科学》2016年第5期63-68,共6页Guizhou Science

摘　　要：贵州下寒武系底部灯影组白云岩之上牛蹄塘组中形成一套分布普遍的黑色页岩,尤其是在贵州遵义地区、贵阳清镇-开阳地区、黔东南施秉-天柱-三穗-麻江一带、黔南三都-都匀-福泉一带、铜仁松桃地区等,以层位稳定特征显著为黑色页岩典型区域。"多金属富矿层"是黑色岩系的重要研究领域,并且取得了长足的发展。系统剖析贵州黑色岩系分布状况和多金属含量特征,结合实际发展需要,探索贵州黑色页岩区的研究尺度,同时也为黑色页岩的研究发展梳理框架与思路。In Guizhou,between the Sinian Dengying Formation and the Niutitang Formation there is a set of black shale rocks,especially in Zunyi,Guiyang-Qingzhen area,Shibing-Tianzhu-Sansui-Majiang area,Sandu- Duyun-Fuquan area and Songtao（ Tongren） area. Polymetallic deposit is very important in the research field of black rock series,and has achieved rapid development. In this paper,we systematically analyzed the distribution of the black rock series and its polymetallic characteristics,explored the research scale of black shale rock area in Guizhou,and cleared the framework of the researches on black shale rock in Guizhou.

关 键 词：黑色岩系 多金属矿床 重金属污染 研究进展 贵州 

分 类 号：P618.2[天文地球—矿床学] X53[天文地球—地质学]