摘要
鹿井矿田是湘赣边高值地质异常带内最重要的局部性致矿异常区.野外解析构造学研究表明，遂川-热水走滑构造直接控制了矿区剪切重熔型岩浆岩、拉分盆地及大型铀矿床的形成和分布重点讨论了走滑断层作用与铀矿质来源、成矿构造条件和成矿媒介条件之间的密切关系，初步提出了鹿井矿区走滑剪切成矿作用模式.
The Lujing ore field is the most important local ore-generating anomaly region within the highvalue geological anomaly zone between eastern Hunan and western Jiangxi provinces. The research into the field analytic tectonics shows that the formation and distribution of shear anatectic magmatic rocks, pull-apart basin and large-sized uranium deposits in the mineralization region were all directly controlled by the SuichuanReshui strike-slip fault structure. The present paper focuses on the close relationship between the strike-slip faulting and the uranium sources, metallogenic tectonic and medium conditions. Finally, this paper proposes the initial pattern of the strike-slip shearing mineralization in the Lujing uranium field.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
1999年第5期476-479,共4页
Earth Science-Journal of China University of Geosciences
基金
国家自然科学基金!49572148
国土资源部矿产资源定量预测及勘查评价开放研究实验室项目
关键词
走滑断层
剪切成矿作用
铀矿田
矿化作用
strike-slip fault, shearing mineralization, Lujing uranium orefield, geological anomaly zone,border region between eastern Hunan and western Jiangxi provinces
