Evidence map›Paper›PMID 41720797›Full record

ArticleNature communications2026

Arc magma formation through the fluid-fluxed mélange melting in subduction zones.

Wei Zhang, Yi-Xiang Chen, Rex N Taylor, Ding-Sheng Jiang, Fang Huang

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Nature communications, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

0numbers the graph read from it
0cells of the map it votes in
0citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

0 citing papers in PubMed.

No citing paper in PubMed yet.

4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

5 authors.

Wei ZhangState Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.
Yi-Xiang ChenState Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China. yxchen07@ustc.edu.cn.ORCID http://orcid.org/0000-0003-4900-4638
Rex N TaylorSchool of Ocean and Earth Science, University of Southampton, Southampton, UK.
Ding-Sheng JiangState Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.
Fang HuangState Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China. fhuang@ustc.edu.cn.ORCID http://orcid.org/0000-0003-1885-3311

Funding

China Postdoctoral Science Foundation 2023M743359National Natural Science Foundation of China (National Science Foundation of China) 42273043National Natural Science Foundation of China (National Science Foundation of China) 42403003National Natural Science Foundation of China (National Science Foundation of China) 92562304
6 · The paper itself

Abstract

The transport of subducted slab materials to the overlying mantle plays a crucial role in arc magma formation. However, the contributions of aqueous fluids, hydrous melts, or mélange to the convective mantle remain controversial due to the lack of definitive fingerprints for these materials. Here, we report the Ba isotope composition of lavas from a typical cold-slab arc, the Izu arc, to resolve the recycled materials in the source of arc magmas. δ

Identifiers

PMID41720797
PMCPMC13043673

What OpenQuestion holds

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Registered trials

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.