| 138铀矿床成矿地质及物化条件分析 |
| |
| 引用本文： | 汤其韬.138铀矿床成矿地质及物化条件分析[J].铀矿地质,1996,12(2):83-90. |
| |
| 作者姓名： | 汤其韬 |
| |
| 作者单位： | 华东地质局２６９大队 |
| |
| 摘 要： | １３８矿床是中生代火山－沉积改造型铀矿床。本文对矿床的铀源、矿区地层岩性、岩相古地理及古气候、构造和改造再生等地质条件，以及铀的吸附还原剂，岩石的有效孔隙度、化学成分、酸碱度、氧化还原电位等物理化学条件进行探讨。
|
| 关 键 词： | 铀矿床，古气候，孔隙度，氧化还原电位 |
ANALYSIS ON METALLOGENETIC GELOGICAL AND PHYSICOCHEMICAL CONDITIONS IN URANIUM DEPOSIT NO. 138 |
| |
| Tang Qitao.ANALYSIS ON METALLOGENETIC GELOGICAL AND PHYSICOCHEMICAL CONDITIONS IN URANIUM DEPOSIT NO. 138[J].Uranium Geology,1996,12(2):83-90. |
| |
| Authors: | Tang Qitao |
| |
| Abstract: | The uranium deposit No. 138 is of Mesozoic volcano-sedimentary transformation type.This paper discusses such geological conditons as source of uranium,stratigraphy and lithology, lithofacies and paleogeography, paleoclimate, structure and reworking-regeneration, and such physicochemical conditions as uranium adsorbent and reductant, effective porosity,chemical compositions,pH and Eh of rocks in the deposit. |
| |
| Keywords: | Uranium deposit Paleoclimate Porosity Redox potential(Eh) |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
