南康市潭口碘矿形成环境分析及成因探讨  

ANALYSIS ON FORMATION ENVIRONMENT OF THE TANKOU IODINE DEPOSIT,NANKANG CITY AND DISCUSSION ON ITS ORIGIN

作　　者：吕少伟 张永忠 

机构地区：[1]江西省地质调查院,江西南昌330201

出　　处：《江西地质》2001年第4期271-275,共5页Jiangxi Geology

摘　　要：本文从红盆地质背景入手,分析了碘富集成矿的水文地质构造环境、有机地球化学环境、古温度环境、电化学作用环境及水文地球化学环境等因素,并在此基础上,对其成因作了初步探讨。Beginning with the geological setting of the red basin,this paper analyzes the hydrogeological structural environment,the organic geochemical environment,the paleotemperature environment,the electro-chemical process environment and hydrogeochemical environment for the enrichment of iodine into ore;and based on this analysis,a preliminary discussion is made on its origin.

关 键 词：碘矿 环境分析 成因 潭口 江西 

分 类 号：P619.211[天文地球—矿床学]