Evidence map›Paper›PMID 31942015›Full record

ArticleScientific reports2020

Discharge of deeply rooted fluids from submarine mud volcanism in the Taiwan accretionary prism.

Nai-Chen Chen, Tsanyao Frank Yang, Wei-Li Hong, Tsai-Luen Yu, In-Tian Lin, Pei-Ling Wang, Saulwood Lin, Chih-Chieh Su, Chuan-Chou Shen, Yunshuen Wang and 1 more

Abstract read
In one paragraph

Article in Scientific reports, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing 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

3 citing papers in PubMed.

  1. Article
  2. Article
  3. 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

11 authors.

Nai-Chen ChenDepartment of Geoscience, National Taiwan University, Taipei, Taiwan.ORCID http://orcid.org/0000-0003-4430-2783
Tsanyao Frank YangDepartment of Geoscience, National Taiwan University, Taipei, Taiwan.
Wei-Li HongGeological Survey of Norway, Trondheim, Norway.
Tsai-Luen YuDepartment of Geoscience, National Taiwan University, Taipei, Taiwan.
In-Tian LinExploration and Development Research Institute, CPC, Taiwan.
Pei-Ling WangResearch Center for Future Earth, National Taiwan University, Taipei, Taiwan.
Saulwood LinInstitute of Oceanography, National Taiwan University, Taipei, Taiwan.
Chih-Chieh SuResearch Center for Future Earth, National Taiwan University, Taipei, Taiwan.ORCID http://orcid.org/0000-0002-7624-1607
Chuan-Chou ShenDepartment of Geoscience, National Taiwan University, Taipei, Taiwan.
Yunshuen WangCentral Geological Survey, MOEA, Taipei, Taiwan.
Li-Hung LinDepartment of Geoscience, National Taiwan University, Taipei, Taiwan. lhlin@ntu.edu.tw.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Qualitative and quantitative assessments of fluid cycling are essential to address the role and transport of deeply sourced fluids in subduction systems. In this study, sediment cores distributed across a submarine mud volcano (SMV) offshore southwestern Taiwan were investigated to determine the characteristics of fluids generated through the convergence between the Eurasian and Phillippine Sea Plates. The low dissolved chloride concentration combined with the enrichment of

Identifiers

PMID31942015
PMCPMC6962449

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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.