Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere
Upward depletion of ophiolitic mantle is produced by melt-peridotite reaction with lateral melt/rock ratio variations in an asthenospheric upwelling column, which flows to become the horizontal oceanic lithospheric mantle under spreading centers.
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2022-11-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-022-34781-w |
| _version_ | 1797984098386444288 |
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| author | Qing Xiong Hong-Kun Dai Jian-Ping Zheng William L. Griffin Hong-Da Zheng Li Wang Suzanne Y. O’ Reilly |
| author_facet | Qing Xiong Hong-Kun Dai Jian-Ping Zheng William L. Griffin Hong-Da Zheng Li Wang Suzanne Y. O’ Reilly |
| author_sort | Qing Xiong |
| collection | DOAJ |
| description | Upward depletion of ophiolitic mantle is produced by melt-peridotite reaction with lateral melt/rock ratio variations in an asthenospheric upwelling column, which flows to become the horizontal oceanic lithospheric mantle under spreading centers. |
| first_indexed | 2024-04-11T06:57:11Z |
| format | Article |
| id | doaj.art-cb7fa912541e4b0a9826f3fe3428c641 |
| institution | Directory Open Access Journal |
| issn | 2041-1723 |
| language | English |
| last_indexed | 2024-04-11T06:57:11Z |
| publishDate | 2022-11-01 |
| publisher | Nature Portfolio |
| record_format | Article |
| series | Nature Communications |
| spelling | doaj.art-cb7fa912541e4b0a9826f3fe3428c6412022-12-22T04:39:01ZengNature PortfolioNature Communications2041-17232022-11-0113111110.1038/s41467-022-34781-wVertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphereQing Xiong0Hong-Kun Dai1Jian-Ping Zheng2William L. Griffin3Hong-Da Zheng4Li Wang5Suzanne Y. O’ Reilly6State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of GeosciencesState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of GeosciencesState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of GeosciencesAustralian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC, School of Natural Sciences, Macquarie UniversityState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of GeosciencesState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of GeosciencesAustralian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC, School of Natural Sciences, Macquarie UniversityUpward depletion of ophiolitic mantle is produced by melt-peridotite reaction with lateral melt/rock ratio variations in an asthenospheric upwelling column, which flows to become the horizontal oceanic lithospheric mantle under spreading centers.https://doi.org/10.1038/s41467-022-34781-w |
| spellingShingle | Qing Xiong Hong-Kun Dai Jian-Ping Zheng William L. Griffin Hong-Da Zheng Li Wang Suzanne Y. O’ Reilly Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere Nature Communications |
| title | Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere |
| title_full | Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere |
| title_fullStr | Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere |
| title_full_unstemmed | Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere |
| title_short | Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere |
| title_sort | vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub spreading center asthenosphere |
| url | https://doi.org/10.1038/s41467-022-34781-w |
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