|本期目录/Table of Contents|

[1]杨中宝,彭省临,胡祥昭,等.浏阳七宝山铜多金属矿床流体包裹体特征及成矿意义[J].地球科学与环境学报,2004,26(02):11-15.
 YANG Zhong-bao,PENG Sheng-lin,HU Xiang-zhao,et al.Ore-forming fluid inclusion characteristics and metallogen of the Qibaoshan Cu-polymetal deposit in Liuyang , Hunan[J].Journal of Earth Sciences and Environment,2004,26(02):11-15.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第26卷
期数:
2004年第02期
页码:
11-15
栏目:
出版日期:
2004-06-20

文章信息/Info

Title:
Ore-forming fluid inclusion characteristics and metallogen of the Qibaoshan Cu-polymetal deposit in Liuyang , Hunan
作者:
杨中宝彭省临胡祥昭李朝艳
中南大学地学与环境工程学院,湖南长沙410083
Author(s):
YANG Zhong-baoPENG Sheng-linHU Xiang-zhaoLI Chao-yan
School ofGeoscience and Environmental Engineering, Central South University, Changsha 410083, China
关键词:
成矿流体包裹体盐度矿化度七宝山湖南浏阳
Keywords:
ore-forming fluidfluid inclusion salinity deg ree of mineralization QibaoshanHunan Liuyang
分类号:
P612
DOI:
-
文献标志码:
A
摘要:
从不同标高、不同矿化带的流体包裹体研究入手,系统地论述了七宝山铜多金属矿床成矿流体 的性质、演化过程及其与成矿的关系。黄铁矿爆裂测温表明:成矿流体温度变化在平面上以岩体为中心 向四周依次为291℃~287℃~279℃,在剖面上由下往上依次为312℃~286℃~228℃。成矿流体 成分主要为H2O,其次为CO2,H+浓度由早期到后期呈递减趋势,表明成矿热液由酸性—弱碱性演化, 同时反映了矿床由高温到中低温的形成过程。
Abstract:
Based on measures of fluid inclusion in different levels and mineralized belt, the characteristics and evolution process of ore-forming fluids in the Qibaoshan Cu-polymetal deposit are discussed systematically. Decrepitation thermomer of pyrite shows temperature of the ore-forming fluids dropped slowly from 291℃ to 279℃ around the rock body in horizontal, and varied from 312℃ to 228℃ from the lower level upward in profile. The main composition of the fluids was H2O and CO2, the concentrations of H+ decrease during evolution of the ore-forming fluids, showing tendency of the fluids from acidity to alkalescence and process of ore-forming.

参考文献/References:

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备注/Memo

备注/Memo:
[收稿日期]2003-04-29
[作者简介]杨中宝1972-),男,云南镇雄人,工程师,博士,现从事地理信息系统与成矿预测研究。
更新日期/Last Update: 2004-06-20