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| DOI | 10.1130/B36847.1 |
| Coexisting Nb-enriched basalts and arc volcanic rocks in the northern Qiangtang Terrane, China: Implications for the effects of ambient mantle on subduction zone magmatism | |
| Zhang, Ze; Chen, Sheng-Sheng; Sun, Da -Wei; Gao, Sen | |
| 发表日期 | 2024 |
| ISSN | 0016-7606 |
| EISSN | 1943-2674 |
| 起始页码 | 136 |
| 结束页码 | 5-6 |
| 卷号 | 136期号:5-6 |
| 英文摘要 | The petrogenesis of Nb-enriched basalts (NEBs) is controversial. NEBs are generally considered to form by melting of either a mixed enriched and depleted mantle source or a mantle wedge metasomatized by adakitic melts. Here we present geochronological, petrological, geochemical, and Sr-Nd-Os isotope data for Early Permian volcanic rocks from the Tuotuohe area in the northern Qiangtang Terrane, China. The studied volcanic rocks can be divided into two groups: arc basalts and basaltic andesites in the lower sequence and NEBs in the upper sequence. Zircon grains from one basaltic andesite sample in the lower sequence yielded a concordia age of 302.0 +/- 1.1 Ma. The geochemical and isotopic characteristics suggest that the NEBs were derived from a mixed source consisting of enriched mid -oceanic ridge basalts (MORB)- to oceanic -island basalt -like ambient mantle and slab -derived fluids, whereas the arc basalts and basaltic andesites originated from a source made of the MORB-type ambient mantle modified by slab -derived melts. We propose for the first time that the Nb enrichment of the NEBs was most likely inherited from high-Nb ambient mantle and is independent of the addition of slab -derived components. In addition to slab -derived components, the nature of the ambient mantle is also an important factor controlling the diversity of arc magmatism. Our new findings show that the Late Carboniferous-Early Permian magmatism in the northern Qiangtang Terrane was related to northward subduction of the Paleo-Tethys Ocean, suggest ing that subduction might have occurred in at least the Early Permian rather than in the previously thought Middle Permian. |
| 语种 | 英语 |
| WOS研究方向 | Geology |
| WOS类目 | Geosciences, Multidisciplinary |
| WOS记录号 | WOS:001234721200004 |
| 来源期刊 | GEOLOGICAL SOCIETY OF AMERICA BULLETIN
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| 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/303597 |
| 作者单位 | China University of Geosciences; China University of Geosciences; Chinese Academy of Sciences; Institute of Tibetan Plateau Research, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS |
| 推荐引用方式 GB/T 7714 | Zhang, Ze,Chen, Sheng-Sheng,Sun, Da -Wei,et al. Coexisting Nb-enriched basalts and arc volcanic rocks in the northern Qiangtang Terrane, China: Implications for the effects of ambient mantle on subduction zone magmatism[J]. 中国科学院青藏高原研究所,2024,136(5-6). |
| APA | Zhang, Ze,Chen, Sheng-Sheng,Sun, Da -Wei,&Gao, Sen.(2024).Coexisting Nb-enriched basalts and arc volcanic rocks in the northern Qiangtang Terrane, China: Implications for the effects of ambient mantle on subduction zone magmatism.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,136(5-6). |
| MLA | Zhang, Ze,et al."Coexisting Nb-enriched basalts and arc volcanic rocks in the northern Qiangtang Terrane, China: Implications for the effects of ambient mantle on subduction zone magmatism".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 136.5-6(2024). |
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