Evidence map›Paper›PMID 37726314›Full record

ArticleNature communications2023

Emplacement of the Argyle diamond deposit into an ancient rift zone triggered by supercontinent breakup.

Hugo K H Olierook, Denis Fougerouse, Luc S Doucet, Yebo Liu, Murray J Rayner, Martin Danišík, Daniel J Condon, Brent I A McInnes, A Lynton Jaques, Noreen J Evans and 5 more

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Nature communications, 2023. 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

15 authors.

Hugo K H OlierookTimescales of Mineral Systems Group, School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia. hugo.olierook@curtin.edu.au.ORCID http://orcid.org/0000-0001-5961-4304
Denis FougerouseSchool of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.ORCID http://orcid.org/0000-0003-3346-1121
Luc S DoucetEarth Dynamics Research Group, School of Earth and Planetary Sciences and The Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.ORCID http://orcid.org/0000-0002-7542-0582
Yebo LiuEarth Dynamics Research Group, School of Earth and Planetary Sciences and The Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.ORCID http://orcid.org/0000-0002-5752-0854
Murray J RaynerRio Tinto, Perth, 6000, Western Australia, Australia.
Martin DanišíkJohn de Laeter Centre, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.ORCID http://orcid.org/0000-0002-0885-4938
Daniel J CondonBritish Geological Survey, Keyworth, Nottingham, NG12 5GG, UK.ORCID http://orcid.org/0000-0002-9082-3283
Brent I A McInnesJohn de Laeter Centre, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.
A Lynton JaquesResearch School of Earth Sciences, Australian National University, Canberra ACT, 2000, Australia.
Noreen J EvansJohn de Laeter Centre, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.ORCID http://orcid.org/0000-0002-7615-8328
Bradley J McDonaldJohn de Laeter Centre, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.
Zheng-Xiang LiEarth Dynamics Research Group, School of Earth and Planetary Sciences and The Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.
Christopher L KirklandTimescales of Mineral Systems Group, School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.ORCID http://orcid.org/0000-0003-3367-8961
Celia MayersJohn de Laeter Centre, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.
Michael T D WingateJohn de Laeter Centre, Curtin University, GPO Box U1987, Perth, WA, 6845, Australia.ORCID http://orcid.org/0000-0003-2528-417X

Funding

Department of Mines, Industry Regulation and Safety, Government of Western Australia (DMIRS) N/A
6 · The paper itself

Abstract

Argyle is the world's largest source of natural diamonds, yet one of only a few economic deposits hosted in a Paleoproterozoic orogen. The geodynamic triggers responsible for its alkaline ultramafic volcanic host are unknown. Here we show, using U-Pb and (U-Th)/He geochronology of detrital apatite and detrital zircon, and U-Pb dating of hydrothermal titanite, that emplacement of the Argyle lamproite is bracketed between 1311 ± 9 Ma and 1257 ± 15 Ma (2σ), older than previously known. To form the Argyle lamproite diatreme complex, emplacement was likely driven by lithospheric extension related to the breakup of the supercontinent Nuna. Extension facilitated production of low-degree partial melts and their migration through transcrustal corridors in the Paleoproterozoic Halls Creek Orogen, a rheologically-weak rift zone adjacent to the Kimberley Craton. Diamondiferous diatreme emplacement during (super)continental breakup may be prevalent but hitherto under-recognized in rift zones at the edges of ancient continental blocks.

Identifiers

PMID37726314
PMCPMC10509175

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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.