中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geochemical constraints on source nature and recycled oceanic crust in the mantle of the Celebes Sea

文献类型:期刊论文

作者Wang, Shuai2,3; Zhang, Guoliang1,3
刊名LITHOS
出版日期2022-06-01
卷号418页码:12
关键词Mantle heterogeneity Eclogite Recycled oceanic crust Olivine Celebes Sea
ISSN号0024-4937
DOI10.1016/j.lithos.2022.106685
通讯作者Zhang, Guoliang(zhangguoliang@qdio.ac.cn)
英文摘要Indian-type mantle is extensively distributed in the marginal basins of the western Pacific; however, the origin of this mantle remains unclear. The Celebes Sea is located between the Pacific and Indian oceans, and its igneous crustal rocks provide crucial constraints on if and on how this anomalous mantle developed in the region. However, limited knowledge has been obtained on the origin of mantle source of the Celebes Sea because only normal-type mid-ocean ridge basalts (N-MORBs) at ODP Site U770 in this basin have been examined. In this study, both N-MORBs and enriched (E)-MORBs were identified at Site U770, which were analyzed for whole-rock major and trace elements, Sr-Nd-Pb-Hf isotopes, and in situ olivine geochemistry. Site U770 basalt samples are Indian-type (i.e., plot above the Northern Hemisphere reference line [NHRL] on plots of 208Pb/204Pb and 207Pb/204Pb versus 206Pb/204Pb) MORBs, based on their Sr-Nd-Pb-Hf isotopic compositions. An enriched mantle end-member exists in the MORB-type depleted mantle source, as evidenced by correlations between epsilon Nd and SmN/YbN, Sr/Sr*, and Eu/Eu*. Recycled igneous oceanic crust that experienced plagioclase fractionation can account for the geochemically enriched end-member in the mantle source, based on the positive correlation of epsilon Nd vs. Sr/Sr* and Eu/Eu*. The recycled igneous oceanic crust plus minor amounts of pelagic sediments can also explain the origins of Indian-type mantle in the Celebes Sea. The E-MORBs have higher Zn/Mn and Zn/Fe ratios, and similar olivine Ni, Ca, and Mn contents as compared to global MORBs, which is also consistent with a recycled oceanic crust-derived, eclogite-rich, mantle source. This suggests recycled components contribute to the lithological and geochemical heterogeneity in the mantle beneath the Celebes Sea.
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDA22050101] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42020302] ; National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41876040] ; Taishan Scholars Program of Shandong Province[tsqn201909157]
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:000799232900003
出版者ELSEVIER
源URL[http://ir.qdio.ac.cn/handle/337002/179323]  
专题海洋研究所_深海极端环境与生命过程研究中心
通讯作者Zhang, Guoliang
作者单位1.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266071, Peoples R China
推荐引用方式
GB/T 7714
Wang, Shuai,Zhang, Guoliang. Geochemical constraints on source nature and recycled oceanic crust in the mantle of the Celebes Sea[J]. LITHOS,2022,418:12.
APA Wang, Shuai,&Zhang, Guoliang.(2022).Geochemical constraints on source nature and recycled oceanic crust in the mantle of the Celebes Sea.LITHOS,418,12.
MLA Wang, Shuai,et al."Geochemical constraints on source nature and recycled oceanic crust in the mantle of the Celebes Sea".LITHOS 418(2022):12.

入库方式: OAI收割

来源:海洋研究所

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