中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sm-Nd age and Sr, Nd isotopic characteristics of the Fanshan potassic alkaline ultramafite-syenite complex in Hebei province, China

文献类型:期刊论文

作者Mu, BL; Shao, JA; Chu, ZY; Yan, GH; Qiao, GS
刊名ACTA PETROLOGICA SINICA
出版日期2001-07-01
卷号17期号:3页码:358-365
关键词alkaline intrusive potassic alkaline layered ultramafite Sm-Nd chronology Sr and Nd isotopes Fanshan intrusive
ISSN号1000-0569
文献子类Article
英文摘要The intrusive complex in the Fanshan, Hebei province, China, consisting of layered patassic alkaline ultramafite and alkaline syenite, is know in the world for its containing large magnetite apatite deposits, and the rocks and deposits have been investigated and a lot of data have been accumulated over the past twenty years. However, their formation timing is still in dispute. Most geologists consider that the rocks and deposits in the Fanshan intrusive complex originated in Triassic Period between 250Ma and 200Ma., but some believe that they were formed in Permian Period. Sm-Nd dating of the Fanshan intrusive complex has been performed, and its age have been obtained. The Sm-Nd isochron age of four mineral samples and two whole rock samples from the Fanshan intrusive complex is 243. 4 +/-9.7Ma with I-Nd = 0.512045, epsilon (Nd) (t) = - 5.4, and the Sm-Nd isochron age of four mineral samples and seven whole rock samples from the Fanshan intrusive complex is 239 +/- 19Ma with I-Nd = 0.512055, epsilon (Nd) (t) = - 5.3 These age data indicate that emplacement of the Fanshan complex started at early Triassic period. However, the Rb-Sr isochron age in the Fanshan complex is 218 +/- 8Ma with I-Sr 0.70554, epsilon (Sr) = 18.4, suggesting possibly that the Fanshan complex was solidified completely in the middle Triassic Period. The Sr, Nd isotope fact of the Fanshan complex above shows that the Fanshan complex was derived from enriched mantle materials.
WOS关键词MANTLE ; GEOCHEMISTRY ; ROCKS ; PB
WOS研究方向Geology
语种英语
WOS记录号WOS:000170244300003
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/76509]  
专题中国科学院地质与地球物理研究所
通讯作者Mu, BL
作者单位1.Beijing Univ, Dept Geol, Beijing 100871, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Mu, BL,Shao, JA,Chu, ZY,et al. Sm-Nd age and Sr, Nd isotopic characteristics of the Fanshan potassic alkaline ultramafite-syenite complex in Hebei province, China[J]. ACTA PETROLOGICA SINICA,2001,17(3):358-365.
APA Mu, BL,Shao, JA,Chu, ZY,Yan, GH,&Qiao, GS.(2001).Sm-Nd age and Sr, Nd isotopic characteristics of the Fanshan potassic alkaline ultramafite-syenite complex in Hebei province, China.ACTA PETROLOGICA SINICA,17(3),358-365.
MLA Mu, BL,et al."Sm-Nd age and Sr, Nd isotopic characteristics of the Fanshan potassic alkaline ultramafite-syenite complex in Hebei province, China".ACTA PETROLOGICA SINICA 17.3(2001):358-365.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

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。