| .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,(1):. |
| 滇西澜沧老厂地区玄武岩岩石成因与构造意义 |
| Petrogenesis and Tectonic Significance of the Laochang Basalt in Western Yunnan Province, China |
| |
| DOI： |
| 中文关键词: 洋岛玄武岩;地球化学;Nd-Pb同位素;滇西 |
| 英文关键词: OIB;geochemistry;Nd-Pb isotope;Western Yunnan Province; |
| 基金项目:中国科学院重要方向项目，国家"973"计划项目 |
|
|
| 摘要点击次数: 1066 |
| 全文下载次数: 0 |
| 中文摘要: |
| 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. |
| 英文摘要: |
| 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. |
|
查看全文
查看/发表评论 下载PDF阅读器 |
| 关闭 |
