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西太平洋采薇海山群基岩特征

韦振权 邓希光 朱克超 姚会强 杨永 任江波

海洋地质前沿2017,Vol.33Issue(12):1-6,6.
海洋地质前沿2017,Vol.33Issue(12):1-6,6.DOI:10.16028/j.1009-2722.2017.12001

西太平洋采薇海山群基岩特征

CHARACTERISTIC OF SUBSTRATE ROCKS OF CAIWEI SEAMOUNTS IN THE WEST PACIFIC OCEAN

韦振权 1邓希光 1朱克超 1姚会强 1杨永 1任江波1

作者信息

  • 1. 国土资源部海底矿产资源重点实验室,中国地质调查局广州海洋地质调查局,广州510075
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摘要

Abstract

Lithology and distribution of substrate rocks of the Caiwei Seamount are scrutinized.Results show that the substrate of the Caiwei Seamounts is mainly composed of pyroclastic rock,limestone,basalt and phosphorite.Pyroclastic rock is the most common one,and basalt and limestone are the second.Phosphorite is seldom.Microscopic examination suggests that pyroclastic rocks are dominated by basaltic volcanic breccias,and limestone is dominated by sparry bioclastic limestone or micritic bioclastic limestone.Phosphorite is mainly formed by phosphatization of bioclastic limestone or volcanic breccia.Preliminary study on geochemistry of basalts from the Caiwei Seamounts shows that the major elements contents of basalts from the Caiwei Seamounts are similar to that of Hawaii alkaline basalts.It suggests that the basalt might be formed in a tectonic environment of alkali island.

关键词

地球化学特征/玄武岩/基岩特征/采薇海山群/西太平洋

Key words

geochemistry/basalt/substrate rock/Caiwei Seamounts/West Pacific Ocean

分类

海洋科学

引用本文复制引用

韦振权,邓希光,朱克超,姚会强,杨永,任江波..西太平洋采薇海山群基岩特征[J].海洋地质前沿,2017,33(12):1-6,6.

基金项目

国家自然科学基金(41606071) (41606071)

国际海域资源调查与开发“十二五”课题(DY125-13-R-05,DY125-13-R-01) (DY125-13-R-05,DY125-13-R-01)

海洋地质前沿

OACSCDCSTPCD

1009-2722

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