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滇西澜沧老厂地区玄武岩岩石成因与构造意义
陈觅; 黄智龙; 罗泰义; 严再飞; 龙汉生
2011
Source Publication矿物学报
Volume31Issue:1Pages:56-61
Other Abstract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。
Keyword洋岛玄武岩 地球化学 Nd-pb同位素 滇西
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:4173022
Citation statistics
Cited Times:1[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7056
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
陈觅,黄智龙,罗泰义,等. 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):56-61.
APA 陈觅,黄智龙,罗泰义,严再飞,&龙汉生.(2011).滇西澜沧老厂地区玄武岩岩石成因与构造意义.矿物学报,31(1),56-61.
MLA 陈觅,et al."滇西澜沧老厂地区玄武岩岩石成因与构造意义".矿物学报 31.1(2011):56-61.
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