Ridge subduction sparked reorganization of the Pacific plate‐mantle system 60–50 million years ago
A reorganization centered on the Pacific plate occurred ~53–47 million years ago. A “top‐down” plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a “bottom‐up” mantle flow mechanism, has been proposed as the main driver. Verification based on marine geophysical observa...
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Published in | Geophysical research letters Vol. 42; no. 6; pp. 1732 - 1740 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Washington
John Wiley & Sons, Inc
28.03.2015
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Subjects | |
Online Access | Get full text |
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Abstract | A reorganization centered on the Pacific plate occurred ~53–47 million years ago. A “top‐down” plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a “bottom‐up” mantle flow mechanism, has been proposed as the main driver. Verification based on marine geophysical observations is impossible as most ocean crust recording this event has been subducted. Using a forward modeling approach, which assimilates surface plate velocities and shallow thermal structure of slabs into mantle flow models, we show that complete Izanagi plate subduction and margin‐wide slab detachment induced a major change in sub‐Pacific mantle flow, from dominantly southward before 60 Ma to north‐northeastward after 50 Ma. Our results agree with onshore geology, mantle tomography, and the inferred motion of the Hawaiian hot spot and are consistent with a plate tectonic process driving the rapid plate‐mantle reorganization in the Pacific hemisphere between 60 and 50 Ma. This reorganization is reflected in tectonic changes in the Pacific and surrounding ocean basins.
Key Points
Pacific Eocene reorganization was triggered by a ridge subduction event
Izanagi plate subduction and slab detachment altered Pacific mantle flow
Our geodynamic models agree with seismic tomography and onshore geology |
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AbstractList | A reorganization centered on the Pacific plate occurred ~53–47 million years ago. A “top‐down” plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a “bottom‐up” mantle flow mechanism, has been proposed as the main driver. Verification based on marine geophysical observations is impossible as most ocean crust recording this event has been subducted. Using a forward modeling approach, which assimilates surface plate velocities and shallow thermal structure of slabs into mantle flow models, we show that complete Izanagi plate subduction and margin‐wide slab detachment induced a major change in sub‐Pacific mantle flow, from dominantly southward before 60 Ma to north‐northeastward after 50 Ma. Our results agree with onshore geology, mantle tomography, and the inferred motion of the Hawaiian hot spot and are consistent with a plate tectonic process driving the rapid plate‐mantle reorganization in the Pacific hemisphere between 60 and 50 Ma. This reorganization is reflected in tectonic changes in the Pacific and surrounding ocean basins. A reorganization centered on the Pacific plate occurred ~53-47million years ago. A "top-down" plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a "bottom-up" mantle flow mechanism, has been proposed as the main driver. Verification based on marine geophysical observations is impossible as most ocean crust recording this event has been subducted. Using a forward modeling approach, which assimilates surface plate velocities and shallow thermal structure of slabs into mantle flow models, we show that complete Izanagi plate subduction and margin-wide slab detachment induced a major change in sub-Pacific mantle flow, from dominantly southward before 60Ma to north-northeastward after 50Ma. Our results agree with onshore geology, mantle tomography, and the inferred motion of the Hawaiian hot spot and are consistent with a plate tectonic process driving the rapid plate-mantle reorganization in the Pacific hemisphere between 60 and 50Ma. This reorganization is reflected in tectonic changes in the Pacific and surrounding ocean basins. A reorganization centered on the Pacific plate occurred ~53-47million years ago. A "top-down" plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a "bottom-up" mantle flow mechanism, has been proposed as the main driver. Verification based on marine geophysical observations is impossible as most ocean crust recording this event has been subducted. Using a forward modeling approach, which assimilates surface plate velocities and shallow thermal structure of slabs into mantle flow models, we show that complete Izanagi plate subduction and margin-wide slab detachment induced a major change in sub-Pacific mantle flow, from dominantly southward before 60Ma to north-northeastward after 50Ma. Our results agree with onshore geology, mantle tomography, and the inferred motion of the Hawaiian hot spot and are consistent with a plate tectonic process driving the rapid plate-mantle reorganization in the Pacific hemisphere between 60 and 50Ma. This reorganization is reflected in tectonic changes in the Pacific and surrounding ocean basins. Key Points * Pacific Eocene reorganization was triggered by a ridge subduction event * Izanagi plate subduction and slab detachment altered Pacific mantle flow * Our geodynamic models agree with seismic tomography and onshore geology A reorganization centered on the Pacific plate occurred ~53–47 million years ago. A “top‐down” plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a “bottom‐up” mantle flow mechanism, has been proposed as the main driver. Verification based on marine geophysical observations is impossible as most ocean crust recording this event has been subducted. Using a forward modeling approach, which assimilates surface plate velocities and shallow thermal structure of slabs into mantle flow models, we show that complete Izanagi plate subduction and margin‐wide slab detachment induced a major change in sub‐Pacific mantle flow, from dominantly southward before 60 Ma to north‐northeastward after 50 Ma. Our results agree with onshore geology, mantle tomography, and the inferred motion of the Hawaiian hot spot and are consistent with a plate tectonic process driving the rapid plate‐mantle reorganization in the Pacific hemisphere between 60 and 50 Ma. This reorganization is reflected in tectonic changes in the Pacific and surrounding ocean basins. Key Points Pacific Eocene reorganization was triggered by a ridge subduction event Izanagi plate subduction and slab detachment altered Pacific mantle flow Our geodynamic models agree with seismic tomography and onshore geology Abstract A reorganization centered on the Pacific plate occurred ~53–47 million years ago. A “top‐down” plate tectonic mechanism, complete subduction of the Izanagi plate, as opposed to a “bottom‐up” mantle flow mechanism, has been proposed as the main driver. Verification based on marine geophysical observations is impossible as most ocean crust recording this event has been subducted. Using a forward modeling approach, which assimilates surface plate velocities and shallow thermal structure of slabs into mantle flow models, we show that complete Izanagi plate subduction and margin‐wide slab detachment induced a major change in sub‐Pacific mantle flow, from dominantly southward before 60 Ma to north‐northeastward after 50 Ma. Our results agree with onshore geology, mantle tomography, and the inferred motion of the Hawaiian hot spot and are consistent with a plate tectonic process driving the rapid plate‐mantle reorganization in the Pacific hemisphere between 60 and 50 Ma. This reorganization is reflected in tectonic changes in the Pacific and surrounding ocean basins. Key Points Pacific Eocene reorganization was triggered by a ridge subduction event Izanagi plate subduction and slab detachment altered Pacific mantle flow Our geodynamic models agree with seismic tomography and onshore geology |
Author | Bower, Dan J. Flament, Nicolas Whittaker, Joanne Müller, R. Dietmar Gurnis, Michael Seton, Maria |
Author_xml | – sequence: 1 givenname: Maria surname: Seton fullname: Seton, Maria organization: University of Sydney – sequence: 2 givenname: Nicolas surname: Flament fullname: Flament, Nicolas organization: University of Sydney – sequence: 3 givenname: Joanne surname: Whittaker fullname: Whittaker, Joanne organization: University of Tasmania – sequence: 4 givenname: R. Dietmar surname: Müller fullname: Müller, R. Dietmar organization: University of Sydney – sequence: 5 givenname: Michael surname: Gurnis fullname: Gurnis, Michael organization: California Institute of Technology – sequence: 6 givenname: Dan J. surname: Bower fullname: Bower, Dan J. organization: California Institute of Technology |
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Snippet | A reorganization centered on the Pacific plate occurred ~53–47 million years ago. A “top‐down” plate tectonic mechanism, complete subduction of the Izanagi... Abstract A reorganization centered on the Pacific plate occurred ~53–47 million years ago. A “top‐down” plate tectonic mechanism, complete subduction of the... A reorganization centered on the Pacific plate occurred ~53-47million years ago. A "top-down" plate tectonic mechanism, complete subduction of the Izanagi... |
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SubjectTerms | Basins Detachment geodynamics Geology Geophysics Hot spots (geology) Izanagi plate Magma Mantle Marine Modelling Movement Ocean basins Ocean models Oceanic crust plate reorganization Plate tectonics Plates (structural members) Plates (tectonics) Recording ridge subduction Ridges Slabs Subduction Subduction (geology) Thermal structure Tomography |
Title | Ridge subduction sparked reorganization of the Pacific plate‐mantle system 60–50 million years ago |
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