Petrogenesis of high-Ti and low-Ti basalts in Emeishan, Yunnan, China.
Jiang HanBing1,2; Jiang ChangYi2; Qian ZhuangZhi2; Zhu Shifei3; Zhang PengBo4; Tang DongMei5
刊名ACTA PETROLOGICA SINICA
2009-05-01
卷号25期号:5页码:1117-1134
关键词Emeishan basalt Petrology Petrogeochemistry Magma process Petrogenesis
ISSN号1000-0569
文献子类Article
英文摘要The most main rock type of the Emeishan basalts are low-Ti basalts and high-Ti basalts, and has the few picrites. They enrich in LILE and LREE at different degrees, and deplete relatively to HREE, REE fractionate evidently, compatible elements (Co, V, Cr, Ni) deplete significantly. Low-Ti basalt magma was obviously contaminated by continent crust, in a larger extent than high-Ti basalt magma. And influences of contamination on Sr isotope and LILE are more evident than those on Nd isotope and REE. Nd and Sr isotope prove that contamination materials are mainly metamorphic rocks of lower continent crust, but also have minor rocks of upper continent crust. That the samples were not contaminated shows Nd and Sr isotopic compositions of moderately depleted mantle. Clinopyroxenes are main fractional crystallization phases/accumulation phases, plagioclases are minor in differentiation processes of high-Mg tholeiitic magma. However, clinopyroxenes and plagioclases are main fractional crystallization phases/accumulation phases of high-Mg transitional magma. Main body part of low-Ti basalts melted around the spinel-garnet transition zone;but main body part of high-Ti basalts melted within the garnet stability field,extremely few are partial melting within the spinel stability field.
WOS关键词PLUME-LITHOSPHERE INTERACTION ; SOUTHWESTERN CHINA ; OCEANIC-CRUST ; FLOOD BASALTS ; PROVINCE ; MANTLE ; VOLCANISM ; EARTH
WOS研究方向Geology
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000266684900007
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/71614]  
专题中国科学院地质与地球物理研究所
通讯作者Jiang HanBing
作者单位1.Xian Inst Geol & Mineral Resources, Xian 710054, Peoples R China
2.Changan Univ, Coll Earth Sci & Land Resourses, Xian 710054, Peoples R China
3.Xian Shiyou Univ, Xian 710065, Peoples R China
4.China Univ Min & Technol, Xuzhou 221008, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Jiang HanBing,Jiang ChangYi,Qian ZhuangZhi,et al. Petrogenesis of high-Ti and low-Ti basalts in Emeishan, Yunnan, China.[J]. ACTA PETROLOGICA SINICA,2009,25(5):1117-1134.
APA Jiang HanBing,Jiang ChangYi,Qian ZhuangZhi,Zhu Shifei,Zhang PengBo,&Tang DongMei.(2009).Petrogenesis of high-Ti and low-Ti basalts in Emeishan, Yunnan, China..ACTA PETROLOGICA SINICA,25(5),1117-1134.
MLA Jiang HanBing,et al."Petrogenesis of high-Ti and low-Ti basalts in Emeishan, Yunnan, China.".ACTA PETROLOGICA SINICA 25.5(2009):1117-1134.
个性服务
查看访问统计
相关权益政策
暂无数据
收藏/分享
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。


©版权所有 ©2017 CSpace - Powered by CSpace