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Contributions of slab-derived fluids to ultrapotassic rocks indicated by K isotopes
Liu, Haiyang1,2,3; Xue, Ying-Yu1,2,3; Wang, Kun1,2,3,5; Sun, Wei-Dong1,2,3,5,6; Wang, Kun4
2021-09-01
发表期刊LITHOS
ISSN0024-4937
卷号396页码:14
通讯作者Liu, Haiyang(hyliu@qdio.ac.cn) ; Xue, Ying-Yu(yingyuxue01@hotmail.com)
摘要Mantle-derived ultrapotassic rocks (K2O/Na2O > 2, K2O > 3 wt%, and MgO > 3 wt%) are crucial to reveal crust mantle interactions. Here, we present petrographic compositions, whole-rock geochemical and potassium (K) isotopic compositions of Baoji ultrapotassic rocks from North Qinling Orogen, China, to trace their origin. The high Ba/La, Ba/Th, Ba/Rb and low Rb/Sr ratios of the investigated ultrapotassic rocks, together with partial melting modelling, reveal a garnet-facies amphibole lherzolite mantle source modified by slab-derived fluids. In particular, the delta K-41 values of the ultrapotassic rocks (-0.57 parts per thousand to -0.06 parts per thousand) are higher than that of the depleted mantle and display positive correlations with K/Th, Ba/Th and Ba/Rb ratios, which indicate that slab-derived fluids have contributed heavy K isotopic signatures to the mantle source from which the ultrapotassic rocks were derived. Collectively, the data demonstrate that slab-derived fluids, or supercritical fluids play important roles in the generation of post-collisional ultrapotassic rocks and K isotopes have the ability to trace the deep processes in subduction zones. (C) 2021 Elsevier B.V. All rights reserved.
关键词K isotopes Ultrapotassic rock Lithospheric mantle Subduction Metasomatism North Qinling Orogen
DOI10.1016/j.lithos.2021.106202
收录类别SCI
语种英语
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDA22050103] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42020303] ; National Natural Science Foundation of China[41903006] ; China Postdoctoral Science Foundation[2019M652497] ; China Postdoctoral Science Foundation[2020T130656] ; postdoctoral innovation project of Shandong province ; postdoctoral applied research program of Qingdao City ; Qingdao National Laboratory for Marine Science and Technology[2017ASTCP-OS07]
WOS研究方向Geochemistry & Geophysics ; Mineralogy
WOS类目Geochemistry & Geophysics ; Mineralogy
WOS记录号WOS:000670300500001
出版者ELSEVIER
引用统计
被引频次:13[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/176949
专题深海极端环境与生命过程研究中心
通讯作者Liu, Haiyang; Xue, Ying-Yu
作者单位1.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, Qingdao 266071, Peoples R China
2.Pilot Natl Lab Marine Sci & Technol Qingdao, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China
3.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China
4.Washington Univ, Dept Earth & Planetary Sci, McDonnell Ctr Space Sci, St Louis, MO 63130 USA
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
6.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
第一作者单位中国科学院海洋研究所;  中国科学院海洋大科学研究中心
通讯作者单位中国科学院海洋研究所;  中国科学院海洋大科学研究中心
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GB/T 7714
Liu, Haiyang,Xue, Ying-Yu,Wang, Kun,et al. Contributions of slab-derived fluids to ultrapotassic rocks indicated by K isotopes[J]. LITHOS,2021,396:14.
APA Liu, Haiyang,Xue, Ying-Yu,Wang, Kun,Sun, Wei-Dong,&Wang, Kun.(2021).Contributions of slab-derived fluids to ultrapotassic rocks indicated by K isotopes.LITHOS,396,14.
MLA Liu, Haiyang,et al."Contributions of slab-derived fluids to ultrapotassic rocks indicated by K isotopes".LITHOS 396(2021):14.
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