Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?
文献类型：期刊论文
| 作者 | Zhang, Yuqi1; Song, Shuguang1; Yang, Liming1; Su, Li2,3; Niu, Yaoling4,5; Allen, Mark B.4; Xu, Xin1
|
| 刊名 | LITHOS
 |
| 出版日期 | 2017-05-01 |
| 卷号 | 278页码:97-110 |
| 关键词 | Picrites Cambrian Oceanic Plateau Trench Jam South Qilian Accretionary Belt Qilian Orogen |
| DOI | 10.1016/j.lithos.2017.01.027 |
| 文献子类 | Article |
| 英文摘要 | Oceanic plateaus with high-Mg rocks in the present-day oceanic crust have attracted much attention for their proposed mantle-plume origins and abnormally high mantle potential temperatures (T-p). However, equivalent rocks in ancient oceanic environments are usually poorly preserved because of deformation and metamorphism. Here we present petrological, geochronological and geochemical data for pillow lavas from Cambrian ophiolites in the Lajishan and Yongjing regions of the South Qilian Accretionary Belt (SQAB), from the southern part of the Qilian Orogen, northern China. Three rock groups can be identified geochemically: (1) sub-alkaline basalts with enriched mid- ocean ridge basalt (E-MORB) affinity; (2) alkaline basalts with oceanic island basalt (OIB) features, probably derived from partial melting of an enriched mantle source; and (3) picrites with MgO (18-22 wt%). Crnumbers [Cr-# = Cr/(Cr + Al)] of spinels from the picrites suggest 18-21% degree of partial melting at the estimated mantle potential temperature (Tp) of 1489-1600 degrees C, equivalent to values of Cenozoic Hawaiian picrites (1500-1600 degrees C). Zircons from one gabbro sample yielded a U-Pb Concordia age of 525 +/- 3 Ma, suggesting the oceanic crust formed in the Cambrian. Available evidence suggests that Cambrian mantle plume activity is preserved in the South Qilian Accretionary Belt, and influenced the regional tectonics: "jamming" of the trench by thick oceanic crust explains the emplacement and preservation of the oceanic plateau, and gave rise to the generation of concomitant Ordovician inner-oceanic island arc basalts via re-organisation of the subduction zones in the region. (C) 2017 Elsevier B.V. All rights reserved. |
| 语种 | 英语 |
| WOS记录号 | WOS:000399258500007 |
| 版本 | 出版稿 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/137042]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 作者单位 | 1.Peking Univ, Sch Earth & Space Sci, MOE Key Lab Orogen Belt & Crustal Evolut, Beijing 100871, Peoples R China 2.China Univ Geosci, Inst Earth Sci, Beijing 100083, Peoples R China 3.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China 4.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England 5.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Yuqi,Song, Shuguang,Yang, Liming,et al. Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?[J]. LITHOS,2017,278:97-110. |
| APA | Zhang, Yuqi.,Song, Shuguang.,Yang, Liming.,Su, Li.,Niu, Yaoling.,...&Xu, Xin.(2017).Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?.LITHOS,278,97-110. |
| MLA | Zhang, Yuqi,et al."Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?".LITHOS 278(2017):97-110. |
入库方式： OAI收割
来源：海洋研究所
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。