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DOI | 10.1016/j.chemgeo.2021.120284 |
Evidence for extreme Sm-Nd fractionation during chemical weathering | |
Feng, Jin-Liang; Zhang, Ji-Feng; Gao, Shao-Peng; Li, Chao-Feng; Ju, Jian-Ting; Liu, Xiao-Ming; Pei, Le-Le; Wang, Kun-Ying | |
通讯作者 | Feng, JL (通讯作者) |
发表日期 | 2021 |
ISSN | 0009-2541 |
EISSN | 1872-6836 |
卷号 | 577 |
英文摘要 | During subaerial chemical weathering, submarine weathering and other intracrustal processes, Sm-Nd chemical fractionation remains uncertain, while a little is known about the conditions, scale and magnitude, specific processes and actual mechanism for possible Sm-Nd fractionation. Here, an in situ terra rossa weathering profile developed on dolostone is chosen for the study. Based on sequential extraction experiments and measurements of the mineral and geochemical compositions including Sr-Nd isotopic compositions, we suggest that subaerial chemical weathering not only leads to considerable Sm-Nd mobilization, redistribution and secondary enrichment, but also gives rise to extreme Sm-Nd fractionation, apparent 143Nd isotope homogenization, nearly complete resetting of the 147Sm-143Nd isotope system, anomalous initial 143Nd/144Nd ratios, and meaningless 143Nd model age (TDM) for weathering products. We found that the lanthanide tetrad effect, rather than mineralogical control, is responsible for the observed substantial Sm-Nd fractionation and for the other rare earth element fractionation. Under domination of the lanthanide tetrad effect, the mobility of Sm is preferential to that of Nd during their migration in the form of dissolved organic complexes. Our results also illustrate that resetting of the 147Sm-143Nd isotope system in weathering products is controlled by the combined effect of the extraneous dissolved Sm-Nd input and additional Sm-Nd fractionation. Finally, we argue that similar scenarios may occur in submarine weathering, diagenesis and other geological processes. |
关键词 | RARE-EARTH-ELEMENTSROSSA OVERLYING DOLOMITEYUNNAN-GUIZHOU PLATEAUTERRA ROSSATRACE-ELEMENTSFERROMANGANESE CONCRETIONSISOTOPIC SYSTEMATICSCONTINENTAL-CRUSTREE FRACTIONATIONBULK COMPOSITION |
英文关键词 | Dolostone; Terra rossa; Chemical weathering; Sm-Nd fractionation; Sm-Nd isotope system; Lanthanide tetrad effect |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000662690400001 |
来源期刊 | CHEMICAL GEOLOGY |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260175 |
推荐引用方式 GB/T 7714 | Feng, Jin-Liang,Zhang, Ji-Feng,Gao, Shao-Peng,et al. Evidence for extreme Sm-Nd fractionation during chemical weathering[J]. 中国科学院青藏高原研究所,2021,577. |
APA | Feng, Jin-Liang.,Zhang, Ji-Feng.,Gao, Shao-Peng.,Li, Chao-Feng.,Ju, Jian-Ting.,...&Wang, Kun-Ying.(2021).Evidence for extreme Sm-Nd fractionation during chemical weathering.CHEMICAL GEOLOGY,577. |
MLA | Feng, Jin-Liang,et al."Evidence for extreme Sm-Nd fractionation during chemical weathering".CHEMICAL GEOLOGY 577(2021). |
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