东坡矿田主要内生矿床成矿规律  

Metallogenetic regularities of main endogenetic deposits in Dongpo orefield,Hunan Province

作　　者：张方军 陈荣华 

机构地区：[1]湖南省地质调查院湘南矿产调查所,湖南郴州423000

出　　处：《华南地质与矿产》2004年第3期38-42,共5页Geology and Mineral Resources of South China

基　　金：中国地质调查局大调查项目(200310200070).

摘　　要：通过对东坡矿田内各主要矿床的产状要素、赋矿标高、硫、铅同位素、测温资料的研究,发现矿田内不同的矿床类型,有它们不同的递温规律、分带规律、台阶规律和侧伏方向。对这一有规律的地质现象的研究可有效控制矿床,对矿床进行合理评价。Study of occurrence, mineralization height, S-Pb isotopes and fluid inclusion homogenization temperatures of main deposits in Dongpo orefield indicates that deposits of different genetic types have different mineralization temperature,zoning regularities, mineralization height and lateral secretion directions. Summarization of these regularities are in favor of effectively controlling and rational evaluating the deposits.

关 键 词：内生矿床 定位系统 东坡矿田 

分 类 号：P612[天文地球—矿床学]