Evidence map›Paper›PMID 35265338›Full record

ArticleNational science review2022

The onset of deep recycling of supracrustal materials at the Paleo-Mesoarchean boundary.

Xiaolei Wang, Ming Tang, Jeff Moyen, Di Wang, Alfred Kröner, Chris Hawkesworth, Xiaoping Xia, Hangqiang Xie, Carl Anhaeusser, Axel Hofmann and 2 more

Open access · goldAbstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in National science review, 2022. 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
3.9field-weighted citation impact, top 6% of its field
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, 27 citations in OpenAlex.

  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

12 authors at 9 institutions in 5 countries.

Xiaolei WangState Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China.ORCID https://orcid.org/0000-0002-5115-7804
Ming TangSchool of Earth and Space Sciences, Peking University, Beijing 100871, China.
Jeff MoyenLaboratoire Magmas et Volcans UMR6524, Université de Lyon, UJM-UCA-CNRS-IRD, Saint Etienne 42023,France.ORCID https://orcid.org/0000-0002-0065-2442
Di WangState Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China.
Alfred KrönerInstitut für Geowissenschaften, Universität Mainz, Mainz 55099, Germany.
Chris HawkesworthDepartment of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK.
Xiaoping XiaState Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.
Hangqiang XieSHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China.
Carl AnhaeusserEconomic Geology Research Unit, University of the Witwatersrand, Johannesburg 2050, South Africa.
Axel HofmannDepartment of Geology, University of Johannesburg, Johannesburg 2006, South Africa.
Junyong LiState Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China.
Linsen LiState Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China.
Nanjing University · CNChinese Academy of Geological Sciences · CNChinese Academy of Sciences · CNJohannes Gutenberg University Mainz · DEPeking University · CNUniversité Claude Bernard Lyon 1 · FRUniversity of Bristol · GBUniversity of Johannesburg · ZAUniversity of the Witwatersrand · ZA

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The recycling of supracrustal materials, and in particular hydrated rocks, has a profound impact on mantle composition and thus on the formation of continental crust, because water modifies the physical properties of lithological systems and the mechanisms of partial melting and fractional fractionation. On the modern Earth, plate tectonics offers an efficient mechanism for mass transport from the Earth's surface to its interior, but how far this mechanism dates back in the Earth's history is still uncertain. Here, we use zircon oxygen (O) isotopes to track recycling of supracrustal materials into the magma sources of early Archean igneous suites from the Kaapvaal Craton, southern Africa. The mean

Indexed as

deep recyclingPaleo-Mesoarchean boundaryplate tectonicsTTGzircon oxygen isotopes

Identifiers

PMID35265338
PMCPMC8900693
OpenAlexW3192348995

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

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.