中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Identifying Crystal Accumulation in Granitoids through Amphibole Composition and In Situ Zircon O Isotopes in North Qilian Orogen

文献类型:期刊论文

作者Chen, Shuo3,4,5; Niu, Yaoling1,2,4; Wang, Xiaohong3,4,5; Xue, Qiqi5; Sun, Wenli6
刊名JOURNAL OF PETROLOGY
出版日期2021-12-01
卷号62期号:12页码:18
关键词amphibole zircon oxygen isotope cumulate granitoids mafic magmatic enclaves (MME)
ISSN号0022-3530
DOI10.1093/petrology/egab096
通讯作者Chen, Shuo(shuochen@qdio.ac.cn)
英文摘要Granitoids are the main constituents of the continental crust, and an understanding of their petrogenesis is key to the origin and evolution of continents. Whether crystal fractionation is the dominant way to generate evolved magmas has long been debated, mostly because such processes would produce large volumes of complementary cumulates, which remains elusive. Mafic magmatic enclaves (MMEs) are ubiquitous in granitoids and their presence was initially recognized as cumulates. However, because many MMEs lack obvious evidence of accumulation, such as the classic cumulate textures and modal layering, the cumulate origin of MMEs has been abandoned and the model of magma mixing between mafic and felsic magmas has become popular. In this study, we conduct a combined study of amphibole composition and in situ O isotopes in zircons on three suites of orogenic granitoids with MMEs from the North Qilian Orogenic Belt (NQOB). We find that the MMEs and their host granodiorites show overlapping zircon delta O-18 values, affirming that they share the same parental magmas. The amphibole compositions indicate that amphiboles from the MMEs are not in equilibrium with a melt whose composition was that of the bulk-rock. These new data, together with the published bulk-rock data, suggest that the MMEs in our study have clear cumulate signatures and are thus of cumulate origin. Our study provides evidence for crystal accumulation in granitoids in the NQOB. This new understanding calls for re-examination on the petrogenesis of some intermediate magmatic rocks (granitoid/andesite) in discussing models of continental crustal growth.
资助项目National Natural Science Foundation (NSFC)[41906050] ; National Natural Science Foundation (NSFC)[41630968] ; National Natural Science Foundation (NSFC)[91958215] ; China Postdoctoral Science Foundation[2019 M652496] ; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1606401] ; Youth Innovation Promotion Association, Chinese Academy of Sciences[2021206] ; 111 project[B18048]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000745055500017
出版者OXFORD UNIV PRESS
源URL[http://ir.qdio.ac.cn/handle/337002/177732]  
专题中国科学院海洋研究所
通讯作者Chen, Shuo
作者单位1.China Univ Geosci, Beijing 100083, Peoples R China
2.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England
3.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China
4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China
5.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
6.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
推荐引用方式
GB/T 7714
Chen, Shuo,Niu, Yaoling,Wang, Xiaohong,et al. Identifying Crystal Accumulation in Granitoids through Amphibole Composition and In Situ Zircon O Isotopes in North Qilian Orogen[J]. JOURNAL OF PETROLOGY,2021,62(12):18.
APA Chen, Shuo,Niu, Yaoling,Wang, Xiaohong,Xue, Qiqi,&Sun, Wenli.(2021).Identifying Crystal Accumulation in Granitoids through Amphibole Composition and In Situ Zircon O Isotopes in North Qilian Orogen.JOURNAL OF PETROLOGY,62(12),18.
MLA Chen, Shuo,et al."Identifying Crystal Accumulation in Granitoids through Amphibole Composition and In Situ Zircon O Isotopes in North Qilian Orogen".JOURNAL OF PETROLOGY 62.12(2021):18.

入库方式: OAI收割

来源:海洋研究所

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