Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
The point in time in which the ancient stagnant-lid tectonic regime with episodic plate subduction changed to continuous plate subduction is still topic of scientific debate. Here, the authors present vast geochemical dataset covering the last 3.5 billion years of Earth’s history and date the onset...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2019-07-01
|
| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-019-11329-z |
| id |
doaj-ba309415c5ec4e6faebfaa1179e70ed7 |
|---|---|
| record_format |
Article |
| spelling |
doaj-ba309415c5ec4e6faebfaa1179e70ed72021-05-11T12:35:44ZengNature Publishing GroupNature Communications2041-17232019-07-011011810.1038/s41467-019-11329-zContinuous plate subduction marked by the rise of alkali magmatism 2.1 billion years agoHe Liu0Wei-dong Sun1Robert Zartman2Ming Tang3Center of Deep-Sea Research, Institute of Oceanology, Chinese Academy of SciencesCenter of Deep-Sea Research, Institute of Oceanology, Chinese Academy of SciencesDepartment of Earth Atmospheric and Planetary Sciences, Massachusetts Institute of TechnologyDepartment of Earth, Environmental and Planetary Sciences, Rice UniversityThe point in time in which the ancient stagnant-lid tectonic regime with episodic plate subduction changed to continuous plate subduction is still topic of scientific debate. Here, the authors present vast geochemical dataset covering the last 3.5 billion years of Earth’s history and date the onset of continuous subduction to about 2.1 billion years ago.https://doi.org/10.1038/s41467-019-11329-z |
| collection |
DOAJ |
| language |
English |
| format |
Article |
| sources |
DOAJ |
| author |
He Liu Wei-dong Sun Robert Zartman Ming Tang |
| spellingShingle |
He Liu Wei-dong Sun Robert Zartman Ming Tang Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago Nature Communications |
| author_facet |
He Liu Wei-dong Sun Robert Zartman Ming Tang |
| author_sort |
He Liu |
| title |
Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago |
| title_short |
Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago |
| title_full |
Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago |
| title_fullStr |
Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago |
| title_full_unstemmed |
Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago |
| title_sort |
continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago |
| publisher |
Nature Publishing Group |
| series |
Nature Communications |
| issn |
2041-1723 |
| publishDate |
2019-07-01 |
| description |
The point in time in which the ancient stagnant-lid tectonic regime with episodic plate subduction changed to continuous plate subduction is still topic of scientific debate. Here, the authors present vast geochemical dataset covering the last 3.5 billion years of Earth’s history and date the onset of continuous subduction to about 2.1 billion years ago. |
| url |
https://doi.org/10.1038/s41467-019-11329-z |
| work_keys_str_mv |
AT heliu continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago AT weidongsun continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago AT robertzartman continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago AT mingtang continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago |
| _version_ |
1721444506481459200 |