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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 |
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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