中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Decoupling of Hf-Nd Isotopes in Challenger Deep Sediments, Mariana Trench: Implications for Sedimentary Hf and Nd Recycling in Subduction Zones

文献类型:期刊论文

作者Pang, Chong-Jin7; Tian, Liyan6; Wang, Xuan-Ce4,5; Zhang, Hanyu6; Wen, Shu-Nv7; Krapez, Bryan7; Liu, Wen-Jing2,3; Liu, Zhi-Xing4; Wu, Tao1
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2021-06-01
卷号126期号:6页码:20
关键词Hf-Nd isotopic decoupling oceanic hydrodynamic mineral sorting sedimentary Hf-Nd recycling density-current deposits Challenger Deep subduction factory
ISSN号2169-9313
DOI10.1029/2021JB021641
英文摘要Decoupling between Hf and Nd isotopes in trench sediments is an important way to produce, via subduction-related recycling, the mantle chemical heterogeneity that is evident in many arc-related magmas. Sediments collected from >7,000 m water depths on the southern and northern slopes of the Challenger Deep were analyzed to understand the factors controlling the variation in Hf and Nd isotopic compositions. These sediments were transported to both flanks of the Challenger Deep by synchronous density currents. All sediment samples show positive e(Hf) values and negative e(Nd) values, mostly plotting above the seawater and terrestrial arrays in Hf-Nd isotope space. Hafnium isotopic compositions in each depositional unit vary (high up to 9.2 e(Hf) units) from lower, coarse-grained laminae to upper, fine-grained graded intervals, showing a good correspondence between e(Hf) values and lamination within depositional units. Such variations are explained by the concentration of Fe-Mn oxyhydroxide-bearing clays in the upper graded intervals, whereas diatom fragments and arc-volcanic detritus are preferentially sorted into lower laminae. These findings demonstrate that the decoupling of Hf-Nd isotopes in trench sediments is not only linked to the nature of provenance but also to hydrodynamic sorting processes during sediment transport. Our results suggest that geographical and stratigraphic variations in sedimentary components (resedimented density-current deposits vs. oceanic pelagites), as well as overall grain size, of the subduction wedge can complicate Hf-Nd isotopic decoupling in resulting arc magmas.
WOS关键词REFERENCE MATERIALS BCR-1 ; IZU-BONIN-MARIANA ; WESTERN PACIFIC ; SM-ND ; SEA SEDIMENTS ; LU-HF ; ELEMENT ; ARC ; GEOCHEMISTRY ; PROVENANCE
资助项目National Natural Science Foundation of China[41973014] ; National Natural Science Foundation of China[41876044] ; Research Start-up Project for Introduced Talent of Yunnan University[20190043] ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)[GML2019ZD0202] ; Youth Innovation Promotion Association CAS[2019067]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000665206200047
出版者AMER GEOPHYSICAL UNION
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Start-up Project for Introduced Talent of Yunnan University ; Research Start-up Project for Introduced Talent of Yunnan University ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Start-up Project for Introduced Talent of Yunnan University ; Research Start-up Project for Introduced Talent of Yunnan University ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Start-up Project for Introduced Talent of Yunnan University ; Research Start-up Project for Introduced Talent of Yunnan University ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Research Start-up Project for Introduced Talent of Yunnan University ; Research Start-up Project for Introduced Talent of Yunnan University ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS
源URL[http://ir.iggcas.ac.cn/handle/132A11/101981]  
专题中国科学院地质与地球物理研究所
通讯作者Pang, Chong-Jin; Wang, Xuan-Ce
作者单位1.Zhejiang Univ, Ocean Coll, Zhoushan, Peoples R China
2.CAS Ctr Excellence Life & Paleoenvironm, Beijing, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
4.Changan Univ, Sch Earth Sci & Resources, Xian, Peoples R China
5.Yunnan Univ, Sch Earth Sci, Kunming, Yunnan, Peoples R China
6.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya, Peoples R China
7.Guilin Univ Technol, Guangxi Key Lab Hidden Metall Ore Deposits Explor, Guilin, Peoples R China
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Pang, Chong-Jin,Tian, Liyan,Wang, Xuan-Ce,et al. Decoupling of Hf-Nd Isotopes in Challenger Deep Sediments, Mariana Trench: Implications for Sedimentary Hf and Nd Recycling in Subduction Zones[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2021,126(6):20.
APA Pang, Chong-Jin.,Tian, Liyan.,Wang, Xuan-Ce.,Zhang, Hanyu.,Wen, Shu-Nv.,...&Wu, Tao.(2021).Decoupling of Hf-Nd Isotopes in Challenger Deep Sediments, Mariana Trench: Implications for Sedimentary Hf and Nd Recycling in Subduction Zones.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,126(6),20.
MLA Pang, Chong-Jin,et al."Decoupling of Hf-Nd Isotopes in Challenger Deep Sediments, Mariana Trench: Implications for Sedimentary Hf and Nd Recycling in Subduction Zones".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 126.6(2021):20.

入库方式: OAI收割

来源:地质与地球物理研究所

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