南华大学学报（自然科学版）Issue(1)：46-52,7.
苗儿山北段深冲铀矿地质特征及成因探讨
Geological Characteristics and Genetic Analysis of Shenchong Uranium Deposit in North Miaoershan Mountain
何友宇 1蒋国清 1刘红兵 1覃金宁1
作者信息
- 1. 湖南省核工业地质局三〇六大队，湖南 衡阳421008
- 折叠
摘要
Abstract
Shenchong mining area in Miaoershan District rich in uranium,is the the origin of granite type uranium deposits. This paper clarifies uranium geology and geochemical characteristics of Shenchong deposits from the geological background,geological character-istics of the deposit,ore minerals compositions,wall rock alteration,characteristics of fluid inclusion,lead isotopic composition and hydrogen and oxygen isotopic composition. It is considered this deposit belongs to cataclastic altered granite type,and its uranium ore-form-ing material source has the characteristics of crust mantle mixing of the uranium deposit which is low temperature and low salinity magmatic hydrothermal uranium deposit.关键词
地质特征/流体包裹体/铅同位素/氢氧同位素/矿床成因Key words
geological characteristics/fluid inclusion/lead isotope/hydrogen and oxygen i-sotope/deposit genesis分类
天文与地球科学引用本文复制引用
何友宇,蒋国清,刘红兵,覃金宁..苗儿山北段深冲铀矿地质特征及成因探讨[J].南华大学学报（自然科学版）,2015,(1):46-52,7.
