IOCAS-IR  > 海洋地质与环境重点实验室
Characteristics of silicon and oxygen isotopic compositions of basalts near East Pacific Rise 13 degrees N
Wang Xiaoyuan1; Zhao Huijing1,2; Zeng Zhigang1; Yin Xuebo1; Chen Shuai1; Ma Yao1,2; Zeng, ZG
2013-12-01
发表期刊ACTA OCEANOLOGICA SINICA
ISSN0253-505X
卷号32期号:12页码:104-108
文章类型Article
摘要In this study, 13 groups of silicon and oxygen isotopes and major elements of the basalts near the East Pacific Rise 13 degrees N are used to study the fractionation of silicon and oxygen isotopes. Among these data, delta Si-30 values of basalts vary from -0.4 parts per thousand to 0.2 parts per thousand with a mean value of delta Si-30 of (-0.18 +/- 0.22)parts per thousand. The delta O-18 values range from 4.1 parts per thousand to 6.4 parts per thousand with a mean delta O-18 value of (+5.35 +/- 0.73)parts per thousand. Since the delta Si-30 values increase in the series of basalt-basaltic andesite- andesite, and delta O-18 values display a positive correlation with the SiO2 content, we propose that the fractionation of silicon and oxygen isotopes is influenced by the SiO2 content in igneous rocks. Compared with the igneous rocks from Manus Basin with clinopyroxene as their dominant mineral phase, MORBs in this study containing olivine and plagioclase as primary minerals have lower delta O-18 and delta Si-30 values, indicating that the fractionation of silicon and oxygen isotopes is also affected by different Si-O bridges in silicate minerals. Furthermore, our samples from the EPR are defined as E-MORB based on K/Ti ratios. Probably, the difference in delta Si-30 and delta O-18 between our samples and a normal MORB are cause by the enriched components in E-MORBs.; In this study, 13 groups of silicon and oxygen isotopes and major elements of the basalts near the East Pacific Rise 13 degrees N are used to study the fractionation of silicon and oxygen isotopes. Among these data, delta Si-30 values of basalts vary from -0.4 parts per thousand to 0.2 parts per thousand with a mean value of delta Si-30 of (-0.18 +/- 0.22)parts per thousand. The delta O-18 values range from 4.1 parts per thousand to 6.4 parts per thousand with a mean delta O-18 value of (+5.35 +/- 0.73)parts per thousand. Since the delta Si-30 values increase in the series of basalt-basaltic andesite- andesite, and delta O-18 values display a positive correlation with the SiO2 content, we propose that the fractionation of silicon and oxygen isotopes is influenced by the SiO2 content in igneous rocks. Compared with the igneous rocks from Manus Basin with clinopyroxene as their dominant mineral phase, MORBs in this study containing olivine and plagioclase as primary minerals have lower delta O-18 and delta Si-30 values, indicating that the fractionation of silicon and oxygen isotopes is also affected by different Si-O bridges in silicate minerals. Furthermore, our samples from the EPR are defined as E-MORB based on K/Ti ratios. Probably, the difference in delta Si-30 and delta O-18 between our samples and a normal MORB are cause by the enriched components in E-MORBs.
关键词Silicon And Oxygen Isotopes Basalt East Pacific Rise Near 13 Degrees n
学科领域Oceanography
DOI10.1007/s13131-013-0396-z
URL查看原文
收录类别SCI
语种英语
WOS研究方向Oceanography
WOS类目Oceanography
WOS记录号WOS:000328528400013
WOS关键词MID-ATLANTIC RIDGE ; PROCESSES BENEATH ; CORE FORMATION ; NAZCA PLATE ; MANTLE ; FRACTIONATION ; HETEROGENEITY ; GEOCHEMISTRY ; SIGNATURES ; EVOLUTION
WOS标题词Science & Technology ; Physical Sciences
引用统计
被引频次:2[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/16292
专题海洋地质与环境重点实验室
通讯作者Zeng, ZG
作者单位1.Chinese Acad Sci, Inst Oceanol, Seafloor Hydrothermal Activ Lab, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
第一作者单位中国科学院海洋研究所
推荐引用方式
GB/T 7714
Wang Xiaoyuan,Zhao Huijing,Zeng Zhigang,et al. Characteristics of silicon and oxygen isotopic compositions of basalts near East Pacific Rise 13 degrees N[J]. ACTA OCEANOLOGICA SINICA,2013,32(12):104-108.
APA Wang Xiaoyuan.,Zhao Huijing.,Zeng Zhigang.,Yin Xuebo.,Chen Shuai.,...&Zeng, ZG.(2013).Characteristics of silicon and oxygen isotopic compositions of basalts near East Pacific Rise 13 degrees N.ACTA OCEANOLOGICA SINICA,32(12),104-108.
MLA Wang Xiaoyuan,et al."Characteristics of silicon and oxygen isotopic compositions of basalts near East Pacific Rise 13 degrees N".ACTA OCEANOLOGICA SINICA 32.12(2013):104-108.
条目包含的文件
文件名称/大小 文献类型 版本类型 开放类型 使用许可
Characteristics of s(377KB) 限制开放CC BY-NC-SA浏览
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Wang Xiaoyuan]的文章
[Zhao Huijing]的文章
[Zeng Zhigang]的文章
百度学术
百度学术中相似的文章
[Wang Xiaoyuan]的文章
[Zhao Huijing]的文章
[Zeng Zhigang]的文章
必应学术
必应学术中相似的文章
[Wang Xiaoyuan]的文章
[Zhao Huijing]的文章
[Zeng Zhigang]的文章
相关权益政策
暂无数据
收藏/分享
文件名: Characteristics of silicon and oxygen isotopic compositions of basalts near East Pacific Rise 13 degrees N.pdf
格式: Adobe PDF
此文件暂不支持浏览
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。