气候变化领域集成服务门户(CCPortal): Grain-scale zircon Hf isotope heterogeneity inherited from sediment-metasomatized mantle: Geochemical and Nd-Hf-Pb-O isotopic constraints on Early Cretaceous intrusions in central Lhasa Terrane, Tibetan Plateau

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DOI	10.2138/am-2022-8508
	Grain-scale zircon Hf isotope heterogeneity inherited from sediment-metasomatized mantle: Geochemical and Nd-Hf-Pb-O isotopic constraints on Early Cretaceous intrusions in central Lhasa Terrane, Tibetan Plateau
	Li, Ming-Jian; Zeng, Yun-Chuan; Tiepolo, Massimo; Farina, Federico; Xu, Ji-Feng; Huang, Feng; Liu, Xi-Jun; Chen, Qin; Ma, Yuan
发表日期	2023
ISSN	0003-004X
EISSN	1945-3027
起始页码	1692
结束页码	1707
卷号	108 期号:9
英文摘要	Clarifying the mechanism of recycling of pre-existing continental crustal materials into the source of mantle-derived magma is a challenging effort that can be of great value to improving our understanding of mantle processes and continental crust growth. This study presents an integrated investigation of whole-rock and mineral geochemical and Nd-Hf-O-Pb isotopic data for dolerites and diorites intruded in the central Lhasa Terrane of Tibetan Plateau at ca. 120 Ma (zircon U-Pb ages). These intrusions have similar distributions of trace elements that are characterized by depletion in Nb-Ta relative to Th, Ba, and U, and moderately negative whole-rock epsilon(Nd)(t) (-5.0 to -1.7) values. Magmatic zircon shows dramatically variable epsilon(Hf)(t) values (from -5.0 to +13.7 in the same rock, including up to 12 epsilon unit variability in single grains). On the other hand, the zircon delta O-18 values are relatively uniform (+6.0%0 to +7.7%0). The constant Pb-208/Pb-206 values of clinopyroxene crystallized at ca. 500-900 MPa suggest no contamination with lower continental crust. The lack of covariation between Hf and O isotopes from the same grains, and the lack of relationship between Hf isotopes and trace elements (e.g., Hf, Th/U, and Yb/Gd) in the magmatic zircons, together with the absence of ancient zircon xenocrysts, imply limited upper crustal contamination. In combination with high-whole-rock Th/La (>0.29) ratios, we interpret the zircon Hf isotope heterogeneity as inherited from a depleted asthenospheric mantle with the addition of 1-4% Hf from isotopically heterogeneous sediments. Our study therefore emphasizes the need for caution when using complex Hf isotopic zonation in zircon as an argument for intracrustal hybridization of two end-member magmas derived from distinct reservoirs. In addition, the high-Zr/Y ratios and no negative Zr-Hf anomalies of the Aruo intrusions imply a high surface temperature of the down going slab that was able to fully dissolve zircons in the subducted sediments. This requires a special geodynamic condition that was most likely related to the steepening of flatly subducted Neo-Tethyan lithosphere at ca. 120 Ma according to a synthesis of regional tectonic-magmatic-sedimentary records.
关键词	Zircon Hf heterogeneity sedimentary recycling mantle metasomatism magma mixing Lhasa Terrane
英文关键词	NUJIANG SUTURE ZONE; U-PB; SOUTHERN TIBET; TRACE-ELEMENT; IN-SITU; CRUSTAL CONTAMINATION; WORKING REFERENCE; MAGMATIC ROCKS; GRANITIC-ROCKS; MC-ICPMS
WOS研究方向	Geochemistry & Geophysics ; Mineralogy
WOS记录号	WOS:001081296900009
来源期刊	AMERICAN MINERALOGIST
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/283882
作者单位	China University of Geosciences - Beijing; University of Milan; Guilin University of Technology
推荐引用方式 GB/T 7714	Li, Ming-Jian,Zeng, Yun-Chuan,Tiepolo, Massimo,et al. Grain-scale zircon Hf isotope heterogeneity inherited from sediment-metasomatized mantle: Geochemical and Nd-Hf-Pb-O isotopic constraints on Early Cretaceous intrusions in central Lhasa Terrane, Tibetan Plateau[J],2023,108(9).
APA	Li, Ming-Jian.,Zeng, Yun-Chuan.,Tiepolo, Massimo.,Farina, Federico.,Xu, Ji-Feng.,...&Ma, Yuan.(2023).Grain-scale zircon Hf isotope heterogeneity inherited from sediment-metasomatized mantle: Geochemical and Nd-Hf-Pb-O isotopic constraints on Early Cretaceous intrusions in central Lhasa Terrane, Tibetan Plateau.AMERICAN MINERALOGIST,108(9).
MLA	Li, Ming-Jian,et al."Grain-scale zircon Hf isotope heterogeneity inherited from sediment-metasomatized mantle: Geochemical and Nd-Hf-Pb-O isotopic constraints on Early Cretaceous intrusions in central Lhasa Terrane, Tibetan Plateau".AMERICAN MINERALOGIST 108.9(2023).