摘要
研究了北阿尔泰地区泥盆纪及石炭纪火山岩的稀土元素特征,并应用稀土判据探讨了区内火山岩的形成机制。稀土元素与常量元素相关关系显示,北阿尔泰泥盆纪及石炭纪火山岩成岩过程中分离结晶作用不明显,其形成机制可能为部分熔融作用。多种稀土元素联合协变关系的研究进一步表明,北阿尔泰泥盆纪及石炭纪火山岩的形成机制为部分熔融作用。同时也显示区内泥盆纪及石炭纪火山岩的稀土元素继承了其源区物质的稀土元素特征。
The characteristics of rare earth elements in the Devonian and Carboniferous volcanic rocks were studied in the north Altay. And the mechanism of formation of volcanic rocks were discussed by using the rare earth elements. The correlativity of rare earth elements and major elements shows that the fractional crystallization is undistinguishable during the formation of Devonian and Carboniferous volcanic rocks, and the mechanism of formation of volcanic rocks may be the partial melting. The further study of the relationship of manifold rare earth elements shows that the mechanism of formation of Devonian and Carboniferous volcanic rocks in the north Altay is the partial melting. And the result also shows that the rare earth elements in the Devonian and Carboniferous volcanic rocks inherited the characteristics of those in its source materiels.
出处
《中国稀土学报》
CAS
CSCD
北大核心
2003年第3期343-347,共5页
Journal of the Chinese Society of Rare Earths
基金
九五"国家科技攻关项目(96 915 02 04
新疆305)
关键词
地球化学
火山岩
形成机制
北阿尔泰
稀土
geochemistry
volcanic rock
mechanism of formation
north Altay
rare earths
