| 安徽沿江成矿带主要控制因素的探讨 |
| |
| 引用本文： | 储国正,曹奋扬.安徽沿江成矿带主要控制因素的探讨[J].安徽地质,2000(1). |
| |
| 作者姓名： | 储国正 曹奋扬 |
| |
| 作者单位： | 安徽省地质矿产局!安徽合肥230001中国地质大学北京 100083(储国正)，安徽省地质矿产局!安徽合肥230001(曹奋扬) |
| |
| 摘 要： | 安徽沿江成矿带是长江中下游铁、铜、硫、金成矿带的重要组成部分。本文依据新的地质、地 球物理和地球化学等资料对安徽沿江地区的深部地质背景、基底地质、构造、岩浆岩及矽卡岩等主要控 矿因素进行了探讨，取得了一些新的进展和新认识。
|
| 关 键 词： | 深部地质背景 基底地质 矽卡岩 花岗岩 安徽沿江成矿带 |
A DISCUSSION ON THE MAJOR CONTROL FACTORS OF THE METALLOGENIC BELT AROUND THE YANGTZE RIVER IN ANHUI |
| |
| CHU Guo-zheng,CAO Fen-yang.A DISCUSSION ON THE MAJOR CONTROL FACTORS OF THE METALLOGENIC BELT AROUND THE YANGTZE RIVER IN ANHUI[J].Geology of Anhui,2000(1). |
| |
| Authors: | CHU Guo-zheng CAO Fen-yang |
| |
| Abstract: | The metallogenic belt around the Yangtze River in Anhui is an important part of the iron, copper, sulphur and gold metallogenic bell of the middle and lower Yangtze River reaches. This paper based on latest geological, geophysical and geochemical data has researched into the deep-seated geological background, basement geology, structure, magmatic rocks and shams around foe Yangtze River in Anhui and made progress with some new knowledge being acquired. |
| |
| Keywords: | deep-seated geologieal background metallogenic belt around the Yangtze River in Anhui basement geology skarns granite |
| 本文献已被 CNKI 等数据库收录！ |
