| 南京汤山膨润土矿地质特征,物化性质及矿床成因 |
| |
| 引用本文： | 陈淑祥 陈克荣. 南京汤山膨润土矿地质特征,物化性质及矿床成因[J]. 高校地质学报, 1998, 4(3): 279-285 |
| |
| 作者姓名： | 陈淑祥 陈克荣 |
| |
| 作者单位： | 南京大学地球科学系 |
| |
| 摘 要： | 通过对南京近郊汤山膨润土矿床的矿区地质、矿床地质特征的分析，阐明了该矿床的成因及其矿石的物化性能。综合研究表明，该矿床是以流纹岩及凝灰岩为成矿原岩，在特定的条件下，经热液蚀变改造而形成的矿床。此矿床之矿石属钙基膨润土，经适当选矿后可用于深加工。
|
| 关 键 词： | 膨润土 矿床成因 地质特征 物化性质 |
| 收稿时间： | 1998-09-20 |
| 修稿时间： | 1998-09-20 |
GEOLOGICAL FEATURES, PHYSICO CHEMICAL PROPERTIES AND GENESIS OF BENTONITE DEPOSIT IN TANGSHAN, NANJING |
| |
| Chen Shuxiang Chen Kerong Zeng Jiahu. GEOLOGICAL FEATURES, PHYSICO CHEMICAL PROPERTIES AND GENESIS OF BENTONITE DEPOSIT IN TANGSHAN, NANJING[J]. Geological Journal of China Universities, 1998, 4(3): 279-285 |
| |
| Authors: | Chen Shuxiang Chen Kerong Zeng Jiahu |
| |
| Affiliation: | Department of Earth Sciences, Nanjing university, Nanjing, 210093 |
| |
| Abstract: | Based on the study of the geological features, the genesis of Tangshan bentonite deposit on the outskirts of Nanjing is elucidated and its physico chemical properties are investigated. The original rocks of the mineral deposit are rhyolite and tuff. Due to hydrothermal alteration under proper conditions the ore can be formed. It is also shown that the bentonites are calcareous ones. After proper ore dressing, the ores can be used for deep procession. |
| |
| Keywords: | Nanjing bentonite depositional origin physico chemical properties of bentonite. |
| 本文献已被 CNKI 维普 等数据库收录！ |
| 点击此处可从《高校地质学报》浏览原始摘要信息 |
|
点击此处可从《高校地质学报》下载全文 |
|
