中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Origin of the Low delta O-18 Signals in Zircons from the Early Cretaceous A-Type Granites in Eastern China: Evidence from the Kulongshan Pluton

文献类型:期刊论文

作者Fan, Wenbo3; Jiang, Neng1,2; Zhai, Mingguo1,2,3; Hu, Jun1,2
刊名JOURNAL OF EARTH SCIENCE
出版日期2021-09-06
页码13
关键词A-type granite low-delta O-18 zircon radiation damage magma derivation
ISSN号1674-487X
DOI10.1007/s12583-021-1515-y
英文摘要The origin of low delta O-18 signals in zircons from the Early Cretaceous A-type granites in eastern China has long been disputed. It is uncertain whether the O-18-depleted features were inherited from high-temperature hydrothermal altered source rock or resulted from water-rock interaction after emplacement. In this paper, zircon oxygen isotopes in the similar to 130 Ma Kulongshan A-type granites in the northern North China Craton are analyzed. The zircons could be subdivided into 5 types based on their luminescent intensity and internal structures in CL images. Their delta O-18 values also vary in different types and show negative correlation with U and Th contents and accompanying cumulative alpha-decay doses, implying that their delta O-18 values may have been modified to various degrees by meteoric water-rock interaction after the accumulation of radiation damage. The idea is further confirmed by oxygen isotopic equilibrium calculation between co-existing mineral pairs. It is inferred that only the least-influenced zircons, with slightly elevated delta O-18 values than normal mantle, have preserved the magmatic oxygen isotopes. In combination with other evidences, it is proposed that the A-type granites are lower-crustal-derived, unnecessarily invoking a high-temperature hydrothermal altered source. The proposition is applicable to many other Cretaceous A-type granites that have similar zircon behaviors.
WOS关键词OXYGEN ISOTOPIC COMPOSITION ; RADIATION-DAMAGE ; NATURAL ZIRCON ; EVOLUTION ; CRATON ; CRUST ; AGE ; MINERALIZATION ; GEOCHRONOLOGY ; PETROGENESIS
资助项目National Natural Science Foundation of China[41973034] ; Postdoctoral Initiation Fund of Northwestern University[208521]
WOS研究方向Geology
语种英语
WOS记录号WOS:000693494800001
出版者CHINA UNIV GEOSCIENCES, WUHAN
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Postdoctoral Initiation Fund of Northwestern University ; Postdoctoral Initiation Fund of Northwestern University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Postdoctoral Initiation Fund of Northwestern University ; Postdoctoral Initiation Fund of Northwestern University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Postdoctoral Initiation Fund of Northwestern University ; Postdoctoral Initiation Fund of Northwestern University ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Postdoctoral Initiation Fund of Northwestern University ; Postdoctoral Initiation Fund of Northwestern University
源URL[http://ir.iggcas.ac.cn/handle/132A11/102648]  
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Fan, Wenbo
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Northwestern Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China
推荐引用方式
GB/T 7714
Fan, Wenbo,Jiang, Neng,Zhai, Mingguo,et al. Origin of the Low delta O-18 Signals in Zircons from the Early Cretaceous A-Type Granites in Eastern China: Evidence from the Kulongshan Pluton[J]. JOURNAL OF EARTH SCIENCE,2021:13.
APA Fan, Wenbo,Jiang, Neng,Zhai, Mingguo,&Hu, Jun.(2021).Origin of the Low delta O-18 Signals in Zircons from the Early Cretaceous A-Type Granites in Eastern China: Evidence from the Kulongshan Pluton.JOURNAL OF EARTH SCIENCE,13.
MLA Fan, Wenbo,et al."Origin of the Low delta O-18 Signals in Zircons from the Early Cretaceous A-Type Granites in Eastern China: Evidence from the Kulongshan Pluton".JOURNAL OF EARTH SCIENCE (2021):13.

入库方式: OAI收割

来源:地质与地球物理研究所

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