中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
In situ geochemical composition of apatite in granitoids from the eastern Central Asian Orogenic Belt: A window into petrogenesis

文献类型:期刊论文

作者Sun, Chen-Yang2,3,4; Cawood, Peter A.3; Xu, Wen-Liang2,5; Zhang, Xiao-Ming2; Tang, Jie2; Li, Yu6; Sun, Zhong-Xing1; Xu, Ting1
刊名GEOCHIMICA ET COSMOCHIMICA ACTA
出版日期2022-01-15
卷号317页码:552-573
关键词Eastern CAOB Erguna and Xing'an massifs Granitoids Apatite Rare earth elements Petrogenesis Adakite
ISSN号0016-7037
DOI10.1016/j.gca.2021.10.028
英文摘要The compositional record of accessory minerals can provide insights into the character and petrogenesis of the parental magma. We demonstrate apatite's applicability to petrogenetic studies through in situ trace element analysis of apatite in 60 granitoid plutons from the eastern Central Asian Orogenic Belt (CAOB). Rare earth element (REE) patterns of apatites usually mimic the trend of the host rock but are slightly enriched in MREE (middle REE), which is predominantly controlled by parental melt composition and REE partitioning. However, the REE patterns of apatites that are decoupled from those of host rocks, such as the depletions of LREE (light REE) and MREE, as well as the HREE (heavy REE) enrichment, result from the early crystallization of other REE-bearing minerals and late-stage metamorphism. Our data displays no significant relationship between apatite trace elements and highly fractionated granitoids in the eastern CAOB, highlighting the limitation of assessing the degree of magma differentiation through apatite geochemistry. More significantly, the variation of Sr in apatite shows a close correlation with the early crystallization of plagioclase, and the linear correlations of Sr-P1-Sr-wR, Sr-P1-Sr-Ap, and Sr-Ap-Sr-wR imply constant Sr partition coefficients of plagioclase and apatite. Furthermore, a partition coefficient of Sr between apatite and bulk rock is proposed (D-Apatite/bulk rock(Sr) = 0.69). Our results also imply that apatite crystallizing from adakites inherits the typical trace element signatures of the adakitic melt and is characterized by high Sr, low HREY (Gd similar to Lu + Y) contents and lack of Eu anomaly. In conclusion, apatite provides a vital bond to understand the petrogenesis of granitoids and shows the potential to track granitic sources in detrital grains. (C) 2021 Elsevier Ltd. All rights reserved.
WOS关键词NE CHINA IMPLICATIONS ; RARE-EARTH-ELEMENTS ; GREAT XINGAN RANGE ; LA-ICP-MS ; TRACE-ELEMENT ; ERGUNA MASSIF ; TECTONIC EVOLUTION ; NORTHEAST CHINA ; PARTITION-COEFFICIENTS ; ISOTOPIC COMPOSITIONS
资助项目National Natural Science Foundation of China[41772047] ; Australian Research Council[LF160100168] ; China Scholarship Council[201906170217] ; Interdisciplinary Research Program for Ph.D. Students of Jilin University[101832020DJX069]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000744072000009
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; China Scholarship Council ; China Scholarship Council ; Interdisciplinary Research Program for Ph.D. Students of Jilin University ; Interdisciplinary Research Program for Ph.D. Students of Jilin University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; China Scholarship Council ; China Scholarship Council ; Interdisciplinary Research Program for Ph.D. Students of Jilin University ; Interdisciplinary Research Program for Ph.D. Students of Jilin University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; China Scholarship Council ; China Scholarship Council ; Interdisciplinary Research Program for Ph.D. Students of Jilin University ; Interdisciplinary Research Program for Ph.D. Students of Jilin University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; China Scholarship Council ; China Scholarship Council ; Interdisciplinary Research Program for Ph.D. Students of Jilin University ; Interdisciplinary Research Program for Ph.D. Students of Jilin University
源URL[http://ir.iggcas.ac.cn/handle/132A11/104027]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Xu, Wen-Liang
作者单位1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
2.Jilin Univ, Coll Earth Sci, 2199 Jianshe St, Changchun 130061, Peoples R China
3.Monash Univ, Sch Earth Atmosphere & Environm, Melbourne, Vic 3800, Australia
4.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China
5.Minist Nat Resources China, Key Lab Mineral Resources Evaluat Northeast Asia, Changchun 130061, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Sun, Chen-Yang,Cawood, Peter A.,Xu, Wen-Liang,et al. In situ geochemical composition of apatite in granitoids from the eastern Central Asian Orogenic Belt: A window into petrogenesis[J]. GEOCHIMICA ET COSMOCHIMICA ACTA,2022,317:552-573.
APA Sun, Chen-Yang.,Cawood, Peter A..,Xu, Wen-Liang.,Zhang, Xiao-Ming.,Tang, Jie.,...&Xu, Ting.(2022).In situ geochemical composition of apatite in granitoids from the eastern Central Asian Orogenic Belt: A window into petrogenesis.GEOCHIMICA ET COSMOCHIMICA ACTA,317,552-573.
MLA Sun, Chen-Yang,et al."In situ geochemical composition of apatite in granitoids from the eastern Central Asian Orogenic Belt: A window into petrogenesis".GEOCHIMICA ET COSMOCHIMICA ACTA 317(2022):552-573.

入库方式: OAI收割

来源:地质与地球物理研究所

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