Evidence map›Paper›PMID 39239122›Full record

ArticleNational science review2024

Correlated crustal and mantle melting documents proto-Tibetan Plateau growth.

Wei Li, Rizheng He, Xiaohui Yuan, Felix Schneider, Frederik Tilmann, Zhen Guo, Yongshun John Chen

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in National science review, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing 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

1 citing paper in PubMed.

  1. Article
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

7 authors.

Wei LiSchool of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China.ORCID https://orcid.org/0000-0002-9428-1784
Rizheng HeSinoProbe Laboratory, Chinese Academy of Geological Sciences, Beijing 100094, China.ORCID https://orcid.org/0000-0002-8054-4723
Xiaohui YuanDeutsches GeoForschungsZentrum GFZ, Potsdam 14473, Germany.ORCID https://orcid.org/0000-0002-2891-1354
Felix SchneiderDeutsches GeoForschungsZentrum GFZ, Potsdam 14473, Germany.
Frederik TilmannDeutsches GeoForschungsZentrum GFZ, Potsdam 14473, Germany.ORCID https://orcid.org/0000-0002-7439-8782
Zhen GuoDepartment of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China.
Yongshun John ChenDepartment of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The mechanism that causes the rapid uplift and active magmatism of the Hoh-Xil Basin in the northern Tibetan Plateau and hence the outward growth of the proto-plateau is highly debated, more specifically, over the relationship between deep dynamics and surface uplift. Until recently the Hoh-Xil Basin remained uncovered by seismic networks due to inaccessibility. Here, based on linear seismic arrays across the Hoh-Xil Basin, we present a three-dimensional S-wave velocity (V

Indexed as

ambient noise tomographyHoh-Xil Basinpartial meltingS-wave velocityTibetan Plateau

Identifiers

PMID39239122
PMCPMC11376070

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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.