Plate Tectonic Oscillations: Unraveling the Wilson Cycle's Deep-Time Geographical Imprint Article Swipe
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· 2025
· Open Access
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· DOI: https://doi.org/10.5281/zenodo.17729822
The Earth's lithosphere is a dynamic system, constantly reshaped by plate tectonics, a process fundamentally described by the Wilson Cycle. This cycle, encompassing the repeated opening and closing of ocean basins and the assembly and breakup of supercontinents, has profoundly influenced Earth's paleogeography over billions of years. While often presented as a straightforward, sequential process, accumulating geological evidence and numerical modeling suggest that the Wilson Cycle is not a monolithic progression but rather exhibits intricate oscillations and variations in its characteristic stages. These oscillations manifest as fluctuations in plate velocities, changes in the timing and nature of subduction initiation, and variations in the geographical distribution and longevity of continental rifting and collision zones. Understanding these deep-time geographical imprints requires a comprehensive synthesis of paleomagnetic data, structural geology, mantle convection models, and geochronological constraints. This paper aims to unravel the nature of these plate tectonic oscillations within the framework of the Wilson Cycle, exploring the underlying geodynamic mechanisms, their observable geological consequences, and their broader implications for Earth system evolution, including climate, sea level, and biodiversity. By recognizing and characterizing these oscillations, we can refine our understanding of supercontinent cycles and gain deeper insights into the complex, episodic nature of Earth's evolving surface and interior.
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- Type
- article
- Landing Page
- https://doi.org/10.5281/zenodo.17729822
- OA Status
- green
- OpenAlex ID
- https://openalex.org/W7107864578
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W7107864578Canonical identifier for this work in OpenAlex
- DOI
-
https://doi.org/10.5281/zenodo.17729822Digital Object Identifier
- Title
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Plate Tectonic Oscillations: Unraveling the Wilson Cycle's Deep-Time Geographical ImprintWork title
- Type
-
articleOpenAlex work type
- Publication year
-
2025Year of publication
- Publication date
-
2025-11-27Full publication date if available
- Authors
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Revista, Zen, GEOGRAPHY, 10List of authors in order
- Landing page
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https://doi.org/10.5281/zenodo.17729822Publisher landing page
- Open access
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YesWhether a free full text is available
- OA status
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greenOpen access status per OpenAlex
- OA URL
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https://doi.org/10.5281/zenodo.17729822Direct OA link when available
- Concepts
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Geology, Supercontinent, Plate tectonics, Lithosphere, Subduction, Paleontology, Geophysics, Mantle convection, Mantle (geology), Tectonics, Paleomagnetism, Breakup, Rift, Geodynamics, Palaeogeography, Continental drift, Polar wander, Mantle plume, Trench, Mid-ocean ridge, Oceanic basin, Lineation, Phanerozoic, Continental margin, Mountain formation, Earth science, Ocean surface topography, Convection, Seafloor spreading, Tethys OceanTop concepts (fields/topics) attached by OpenAlex
- Cited by
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0Total citation count in OpenAlex
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| abstract_inverted_index.collision | 111 |
| abstract_inverted_index.deep-time | 115 |
| abstract_inverted_index.described | 15 |
| abstract_inverted_index.exploring | 152 |
| abstract_inverted_index.framework | 147 |
| abstract_inverted_index.including | 169 |
| abstract_inverted_index.interior. | 203 |
| abstract_inverted_index.intricate | 74 |
| abstract_inverted_index.longevity | 106 |
| abstract_inverted_index.numerical | 59 |
| abstract_inverted_index.presented | 49 |
| abstract_inverted_index.synthesis | 121 |
| abstract_inverted_index.constantly | 7 |
| abstract_inverted_index.convection | 128 |
| abstract_inverted_index.evolution, | 168 |
| abstract_inverted_index.geodynamic | 155 |
| abstract_inverted_index.geological | 56, 159 |
| abstract_inverted_index.influenced | 40 |
| abstract_inverted_index.monolithic | 69 |
| abstract_inverted_index.observable | 158 |
| abstract_inverted_index.profoundly | 39 |
| abstract_inverted_index.sequential | 53 |
| abstract_inverted_index.structural | 125 |
| abstract_inverted_index.subduction | 97 |
| abstract_inverted_index.tectonics, | 11 |
| abstract_inverted_index.underlying | 154 |
| abstract_inverted_index.variations | 77, 100 |
| abstract_inverted_index.continental | 108 |
| abstract_inverted_index.initiation, | 98 |
| abstract_inverted_index.lithosphere | 2 |
| abstract_inverted_index.mechanisms, | 156 |
| abstract_inverted_index.progression | 70 |
| abstract_inverted_index.recognizing | 176 |
| abstract_inverted_index.velocities, | 89 |
| abstract_inverted_index.accumulating | 55 |
| abstract_inverted_index.constraints. | 132 |
| abstract_inverted_index.distribution | 104 |
| abstract_inverted_index.encompassing | 22 |
| abstract_inverted_index.fluctuations | 86 |
| abstract_inverted_index.geographical | 103, 116 |
| abstract_inverted_index.implications | 164 |
| abstract_inverted_index.oscillations | 75, 83, 144 |
| abstract_inverted_index.Understanding | 113 |
| abstract_inverted_index.biodiversity. | 174 |
| abstract_inverted_index.comprehensive | 120 |
| abstract_inverted_index.consequences, | 160 |
| abstract_inverted_index.fundamentally | 14 |
| abstract_inverted_index.oscillations, | 180 |
| abstract_inverted_index.paleomagnetic | 123 |
| abstract_inverted_index.understanding | 185 |
| abstract_inverted_index.characteristic | 80 |
| abstract_inverted_index.characterizing | 178 |
| abstract_inverted_index.paleogeography | 42 |
| abstract_inverted_index.supercontinent | 187 |
| abstract_inverted_index.geochronological | 131 |
| abstract_inverted_index.straightforward, | 52 |
| abstract_inverted_index.supercontinents, | 37 |
| cited_by_percentile_year | |
| countries_distinct_count | 0 |
| institutions_distinct_count | 2 |
| citation_normalized_percentile.value | 0.73956976 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |