| 滇西澜沧老厂地区玄武岩岩石成因与构造意义 |
| |
| 引用本文： | 陈觅,黄智龙,罗泰义,严再飞,龙汉生.滇西澜沧老厂地区玄武岩岩石成因与构造意义[J].矿物学报,2011,31(1):55-61. |
| |
| 作者姓名： | 陈觅 黄智龙 罗泰义 严再飞 龙汉生 |
| |
| 作者单位： | 1. 中国科学院地球化学研究所矿床地球化学国家重点实验室,贵州,贵阳,550002;中国科学院研究生院,北京,100049
2. 中国科学院地球化学研究所矿床地球化学国家重点实验室,贵州,贵阳,550002 |
| |
| 基金项目： | 中国科学院重要方向项目，国家"973"计划项目 |
| |
| 摘 要： | 对滇西澜沧老厂地区玄武岩进行了系统的主微量元素和Nd-Pb同位素地球化学研究,结果表明该玄武岩为典型的洋岛玄武岩(OIB)。Nd-Pb同位素研究表明,玄武岩浆含富集地幔组分。老厂地区玄武岩浆活动可能与地幔热柱有关,玄武岩可能为地幔热柱(软流圈)熔融产生的岩浆与富集的岩石圈地幔岩浆混合的产物。
|
| 关 键 词： | 洋岛玄武岩 地球化学 Nd-Pb同位素 滇西 |
Petrogenesis and Tectonic Significance of the Laochang Basalt in Western Yunnan Province, China |
| |
| CHEN Mi,HUANG Zhi-long,LUO Tai-yi,YAN Zai-fei,LONG Han-sheng.Petrogenesis and Tectonic Significance of the Laochang Basalt in Western Yunnan Province, China[J].Acta Mineralogica Sinica,2011,31(1):55-61. |
| |
| Authors: | CHEN Mi HUANG Zhi-long LUO Tai-yi YAN Zai-fei LONG Han-sheng |
| |
| Institution: | CHEN Mi1,2,HUANG Zhi-long1,LUO Tai-yi1,YAN Zai-fei1,LONG Han-sheng1,2(1.State Key Laboratory of Ore Deposits Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China,2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China) |
| |
| Abstract: | A systematic investigation on major and trace elements and Nd-Pb isotope geochemistry date of the Laochang basalt in western Yunnan Province shows that the basalt is a typical oceanic island basalt(OIB).Nd-Pb isotope data revealed that basaltic magma contained enriched mantle component.The basaltic magma activity in Laochang may be related to mantle plume,and the basalt may be the mixed products of mantle plume(asthenosphere) melting of the magma and enriched lithospheric mantle magma. |
| |
| Keywords: | OIB geochemistry Nd-Pb isotope Western Yunnan Province |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
|
