| 湘南内生锡矿的成矿构造-地球化学类型 |
| |
| 引用本文： | 徐惠长,王红霞,李建中.湘南内生锡矿的成矿构造-地球化学类型[J].华南地质与矿产,2006(1):1-7. |
| |
| 作者姓名： | 徐惠长 王红霞 李建中 |
| |
| 作者单位： | 湖南省湘南地质勘察院,湖南,郴州,423000 |
| |
| 基金项目： | 中国主要成矿区带研究项目 |
| |
| 摘 要： | 以地质构造特征和锡矿的富集规律为依据,对湘南地区内生锡矿的构造-地球化学类型进行了研究和划分.认为湘南内生锡矿主要形成于燕山期,属于造山带型中酸性-酸性岩浆成矿建造,其成矿构造-地球化学类型为陆内板块拼贴带亲氧型、亲铁-亲硫型和走滑断裂带亲硫-亲氧型.
|
| 关 键 词： | 内生锡矿 构造-地球化学类型 湘南 |
| 文章编号： | 1007-3701（2006）01-0001-07 |
| 收稿时间： | 2005-04-18 |
| 修稿时间： | 2005年4月18日 |
Metallotectonics-geochemistry type of the endogenetic tin ore deposit in south Hunan province |
| |
| Xu Hui-chang,Wang Hong-xia,Li Jian-zhong.Metallotectonics-geochemistry type of the endogenetic tin ore deposit in south Hunan province[J].Geology and Mineral Resources of South China,2006(1):1-7. |
| |
| Authors: | Xu Hui-chang Wang Hong-xia Li Jian-zhong |
| |
| Abstract: | Based on the geological structural characteristic and the rule of the tin ore concentration in south Hunan, the authors discuss and subdivide the structure-geochemical type of the tin ore deposit. It is showing that the main formation of the tin ore deposit are Yanshanian, belonging to the intermediate-acidiy rock-acid magmatic formation in south Hunan. The ore-forming structure-geochemical type can be subdivided into the oxyphile, siderophile-chalcophile type in plate junction of inner continental plate and the oxyphilechalcophile type in the flaw fault zone. |
| |
| Keywords: | endogenetic tin ore deposit structure - geochemistry types south Hunan provice |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
