Origins of plate tectonics.

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Title: Origins of plate tectonics.
Authors: P. G.
Source: Proceedings of the National Academy of Sciences of the United States of America. 3/10/2026, Vol. 123 Issue 10, p1-1. 1p.
Subjects: Plate tectonics, Hadean, Precambrian, Minerals
Geographic Terms: Australia
Abstract: The article focuses on research into the origins of Earth's plate tectonics by analyzing zircon crystals from Jack Hills, Australia, which date back over 4 billion years. The study found that the igneous cores of these zircons indicate a moderately oxidized mantle source during the Hadean Eon, suggesting early mantle convection. Metamorphic rims of the crystals reveal temperature and pressure conditions consistent with modern plate tectonics beginning by the Archean Eon, around 3.35 billion years ago. These findings imply that Earth's mantle reached near-modern oxidation states by approximately 4.15 billion years ago, supporting the emergence of collisional tectonics in the early Earth. [Extracted from the article]
Copyright of Proceedings of the National Academy of Sciences of the United States of America is the property of National Academy of Sciences and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
Database: Engineering Source
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DbLabel: Engineering Source
An: 192507569
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PubType: Academic Journal
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  Data: The article focuses on research into the origins of Earth's plate tectonics by analyzing zircon crystals from Jack Hills, Australia, which date back over 4 billion years. The study found that the igneous cores of these zircons indicate a moderately oxidized mantle source during the Hadean Eon, suggesting early mantle convection. Metamorphic rims of the crystals reveal temperature and pressure conditions consistent with modern plate tectonics beginning by the Archean Eon, around 3.35 billion years ago. These findings imply that Earth's mantle reached near-modern oxidation states by approximately 4.15 billion years ago, supporting the emergence of collisional tectonics in the early Earth. [Extracted from the article]
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  Data: <i>Copyright of Proceedings of the National Academy of Sciences of the United States of America is the property of National Academy of Sciences and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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        Value: 10.1073/iti1026123
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        Text: English
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      – SubjectFull: Plate tectonics
        Type: general
      – SubjectFull: Hadean
        Type: general
      – SubjectFull: Precambrian
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      – SubjectFull: Minerals
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              Text: 3/10/2026
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