摘要
板块构造学说推动了玄武岩理论的完善和进步,从20世纪70年代兴起的玄武岩构造环境判别方法成为学术界关注的热点,虽然现在逐渐降温了,但在国内仍然倍受青睐。大洋中脊玄武岩(MORB)是拥有数据最多、数据质量最好、研究得最详细的玄武岩类,是构建玄武岩理论的基石。本文利用Pet DB数据库资料(http://www.earthchem.org/petdb/search),对全球MORB数据进行了初步的挖掘,发现早先的玄武岩构造环境判别方法的理论、思路需要进一步的完善。早先研究认为,N-MORB是强烈亏损的。但本文研究却显示,MORB成分具有较宽的变化范围,包含了从MORB到OIB及IAB的组分,即部分MORB并不是亏损的,而是相对富集的。因此,玄武岩构造环境判别理论及方法有待进一步的完善。
The plate tectonic hypothesis enriched basalt theory. The basalt tectonic discrimination diagrams which raised in 1970s had been a hot topic for decades although it is much less popular as before, however, the method is still favored by some domestic scholars. Mid-Ocean Ridge Basalt (MORB) was the footstone for the basalt theory. This study presented an initial data mining based on the PetDB database (http://www.earthchem.org/petdb/search) which showed that the past basalt tectonic discrimination diagrams should be updated. The previous studies considered that N-MORB is strong depleted in large ion lithophile elements, however, this study suggested that the N-MORBs have highly varied components. Therefore, the basalt tectonic environment discrimination method should be further improved and cautions must be taken in using of the discrimination diagrams.
出处
《大地构造与成矿学》
EI
CAS
CSCD
北大核心
2017年第2期420-431,共12页
Geotectonica et Metallogenia
基金
中央高校基本科研业务费项目(Lzu-Jbky-2012-128)
中国科学院地质与地球物理研究所岩石圈演化国家重点实验室项目(81300001)联合资助