贵州滑石矿床类型及找矿标志 |
| |
引用本文: | 谢宏.贵州滑石矿床类型及找矿标志[J].建材地质,2012(3):57-59. |
| |
作者姓名: | 谢宏 |
| |
作者单位: | 贵州大学资源与环境工程学院,贵州贵阳550003 |
| |
摘 要: | 贵州的滑石矿床根据其成矿地质条件可分为沉积型和中低温热液型两种类型。沉积型滑石矿床产于碳酸盐岩建造中,层位稳定、厚度较大。与超基性岩建造有关的中低温热液型滑石矿脉规模小、变化大,但矿石质量较好。通过研究滑石矿床地质特征,进一步总结了区域找矿标志。
|
关 键 词: | 滑石 矿床类型 找矿标志 贵州 |
Types of Talc Deposits in Guizhou and Their Prospecting Indications |
| |
Authors: | XIE Hong |
| |
Affiliation: | XIE Hong (Institute of Resource and Environment, Guizhou University, Guiyang 550003, China) |
| |
Abstract: | Based on metallogenic factors, the talc deposits in Guizhou can be classified into two types: sedimentary type and meso-epi-thermal type. The sedimentary type talc deposits occur in carbonate formation. The meso-epi-thermal type talc deposits pertain to the ultrabasic formation have small-scale.The regional prospecting indications of talc deposits are also summarized in this paper researching on geology characteristics. |
| |
Keywords: | talc deposit deposit type prospecting indication Guizhou |
本文献已被 维普 等数据库收录! |
|