Post-collisional magmatism: Consequences of UHPM terrane exhumation and orogen collapse, N. Qaidam UHPM belt, NW China
文献类型：期刊论文
| 作者 | Wang, Mengjue1; Song, Shuguang1,2; Niu, Yaoling2,3; Su, Li4 |
| 刊名 | LITHOS
 |
| 出版日期 | 2014-12-01 |
| 卷号 | 210页码:181-198 |
| 关键词 | Post-collisional magmatism UHPM terrane Exhumation and extensional collapse Mantle upwelling North Qaidam |
| 通讯作者 | Song, SG (reprint author), Peking Univ, Sch Earth & Space Sci, MOE Key Lab Orogen Belt & Crustal Evolut, Beijing 100871, Peoples R China. |
| 英文摘要 | Exhumation of subducted slabs and extensional collapse of orogens are the main tectonic processes in ancient and modern continental collisional zones. Magmatism during these two processes may play important roles in understanding reworking and growth of the continental crust We report here that a series of plutonic magmas, including intrusions of two-mica granite, tonalite, granodiorite, biotite monzogranite, porphyritic biotite granite and diorite, as well as contemporaneous mafic dykes, have been recognized in Dulan edogite-bearing terrane, the North Qaidam ultra-high pressure metamorphic (UHPM) belt The magmatism represented by these plutons is temporally similar to 20-30 million years (Mys) younger than the UHPM age, lasting for similar to 40 Mys and derived from different sources with different mechanisms. The magmatism was initiated by exhumation of UHPM terranes during which strongly-peraluminous two-mica granite and metaluminous tonalite were produced respectively by decompression melting of the exhumed UHPM upper and lower continental crust, respectively. The genesis of mafic magmatic enclave (MME)-hosting granodiorite with a clear hybrid signature and coeval biotite monzogranite reflected the upwelling of asthenospheric mantle by extension of lithosphere during the orogen collapse. It was induced by detachment of the subducted lithospheric mantle, which then brought heat and mantle material into continental crust and triggered the partial melting of the exhumed UHPM continental crust, and gave rise to mixing of crustal and mantle melts. Porphyritic biotite granite reflects a late melting event of continental crust Diorite marked by high magnesium content represents mantle melts with slight crustal contamination, which implies that the orogen has been unrooted and collapsed completely. The post-collisional magmatism of the North Qaidam belt provides an improved understanding for the late thermal and tectonic evolution of a UHPM continental collision zone. (C) 2014 Elsevier B.V. All rights reserved. |
| 学科主题 | Geochemistry & Geophysics; Mineralogy |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000347507600012 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/23833]  |
| 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.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England 3.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 4.China Univ Geosci, Inst Earth Sci, Beijing 100083, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Mengjue,Song, Shuguang,Niu, Yaoling,et al. Post-collisional magmatism: Consequences of UHPM terrane exhumation and orogen collapse, N. Qaidam UHPM belt, NW China[J]. LITHOS,2014,210:181-198. |
| APA | Wang, Mengjue,Song, Shuguang,Niu, Yaoling,&Su, Li.(2014).Post-collisional magmatism: Consequences of UHPM terrane exhumation and orogen collapse, N. Qaidam UHPM belt, NW China.LITHOS,210,181-198. |
| MLA | Wang, Mengjue,et al."Post-collisional magmatism: Consequences of UHPM terrane exhumation and orogen collapse, N. Qaidam UHPM belt, NW China".LITHOS 210(2014):181-198. |
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。