Plate Tectonic Metamorphosis: Subduction-to-Ridge Transitions and the Wilsonian Remapping of Earth's Surface Article Swipe
Revista, Zen
,
GEOGRAPHY, 10
·
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.5281/zenodo.17728097
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.5281/zenodo.17728097
Plate tectonics is the fundamental framework for understanding Earth's dynamic surface processes, dictating the creation, consumption, and redistribution of lithosphere. While divergent (mid-ocean ridges) and convergent (subduction zones) plate boundaries are typically viewed as distinct and relatively stable features, the transition of a subduction zone into a spreading ridge, or vice versa, represents a profound tectonic metamorphosis with significant implications for global geodynamics and surface evolution. This paper explores the mechanisms and consequences of such subduction-to-ridge transitions, examining how these events contribute to the Wilsonian remapping of Earth's surface. We review the geological and geophysical evidence for ridge subduction, slab window formation, and the subsequent initiation of new spreading centers or the demise of existing ones. Key case studies, such as the evolution of the Pacific Ring of Fire and the tectonic history of various triple junctions, are analyzed to illustrate the complex interplay of plate kinematics, mantle dynamics, and crustal deformation during these transformative events. We propose that these transitions are not merely localized phenomena but are integral to the larger supercontinent cycle, driving major shifts in plate configurations, magmatism, and orogenesis. Understanding the drivers and signatures of subduction-to-ridge metamorphosis is crucial for refining paleogeographic reconstructions, deciphering the long-term evolution of Earth's mantle convection, and predicting future geological activity.
Related Topics
Concepts
Plate tectonics
Geology
Geodynamics
Subduction
Supercontinent
Tectonics
Mantle (geology)
Paleontology
Geophysics
Overprinting
Mid-ocean ridge
Convergent boundary
Oceanic crust
Slab
Transition zone
Seismology
Crust
Ridge
Lithosphere
Slab window
Mantle convection
Geologic record
Early Earth
Trench
Planet
Metadata
- Type
- article
- Landing Page
- https://doi.org/10.5281/zenodo.17728097
- OA Status
- green
- OpenAlex ID
- https://openalex.org/W7106819314
All OpenAlex metadata
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https://openalex.org/W7106819314Canonical identifier for this work in OpenAlex
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https://doi.org/10.5281/zenodo.17728097Digital Object Identifier
- Title
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Plate Tectonic Metamorphosis: Subduction-to-Ridge Transitions and the Wilsonian Remapping of Earth's SurfaceWork title
- Type
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articleOpenAlex work type
- Publication year
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2025Year of publication
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2025-11-26Full publication date if available
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Revista, Zen, GEOGRAPHY, 10List of authors in order
- Landing page
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https://doi.org/10.5281/zenodo.17728097Publisher landing page
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YesWhether a free full text is available
- OA status
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greenOpen access status per OpenAlex
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https://doi.org/10.5281/zenodo.17728097Direct OA link when available
- Concepts
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Plate tectonics, Geology, Geodynamics, Subduction, Supercontinent, Tectonics, Mantle (geology), Paleontology, Geophysics, Overprinting, Mid-ocean ridge, Convergent boundary, Oceanic crust, Slab, Transition zone, Seismology, Crust, Ridge, Lithosphere, Slab window, Mantle convection, Geologic record, Early Earth, Trench, PlanetTop concepts (fields/topics) attached by OpenAlex
- Cited by
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0Total citation count in OpenAlex
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| abstract_inverted_index.convergent | 25 |
| abstract_inverted_index.evolution. | 65 |
| abstract_inverted_index.formation, | 101 |
| abstract_inverted_index.geological | 92, 208 |
| abstract_inverted_index.illustrate | 140 |
| abstract_inverted_index.initiation | 105 |
| abstract_inverted_index.junctions, | 136 |
| abstract_inverted_index.magmatism, | 180 |
| abstract_inverted_index.mechanisms | 70 |
| abstract_inverted_index.predicting | 206 |
| abstract_inverted_index.processes, | 11 |
| abstract_inverted_index.relatively | 36 |
| abstract_inverted_index.represents | 52 |
| abstract_inverted_index.signatures | 187 |
| abstract_inverted_index.subduction | 43 |
| abstract_inverted_index.subsequent | 104 |
| abstract_inverted_index.transition | 40 |
| abstract_inverted_index.(subduction | 26 |
| abstract_inverted_index.convection, | 204 |
| abstract_inverted_index.deciphering | 197 |
| abstract_inverted_index.deformation | 151 |
| abstract_inverted_index.fundamental | 4 |
| abstract_inverted_index.geodynamics | 62 |
| abstract_inverted_index.geophysical | 94 |
| abstract_inverted_index.kinematics, | 146 |
| abstract_inverted_index.orogenesis. | 182 |
| abstract_inverted_index.significant | 58 |
| abstract_inverted_index.subduction, | 98 |
| abstract_inverted_index.transitions | 160 |
| abstract_inverted_index.consequences | 72 |
| abstract_inverted_index.consumption, | 15 |
| abstract_inverted_index.implications | 59 |
| abstract_inverted_index.lithosphere. | 19 |
| abstract_inverted_index.transitions, | 76 |
| abstract_inverted_index.Understanding | 183 |
| abstract_inverted_index.metamorphosis | 56, 190 |
| abstract_inverted_index.understanding | 7 |
| abstract_inverted_index.redistribution | 17 |
| abstract_inverted_index.supercontinent | 172 |
| abstract_inverted_index.transformative | 154 |
| abstract_inverted_index.configurations, | 179 |
| abstract_inverted_index.paleogeographic | 195 |
| abstract_inverted_index.reconstructions, | 196 |
| abstract_inverted_index.subduction-to-ridge | 75, 189 |
| cited_by_percentile_year | |
| countries_distinct_count | 0 |
| institutions_distinct_count | 2 |
| citation_normalized_percentile.value | 0.81995471 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |