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Nathaniel Butterworth
Researcher at University of Sydney
Publications - 15
Citations - 494
Nathaniel Butterworth is an academic researcher from University of Sydney. The author has contributed to research in topics: Subduction & Slab. The author has an hindex of 9, co-authored 15 publications receiving 377 citations.
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Abrupt plate accelerations shape rifted continental margins
TL;DR: Rifted margins feature an initial, slow rift phase and that an abrupt increase of plate divergence introduces a fast rift phase, and it is demonstrated that abrupt plate acceleration during continental rifting is controlled by the nonlinear decay of the resistive rift strength force.
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Geological, tomographic, kinematic and geodynamic constraints on the dynamics of sinking slabs
Nathaniel Butterworth,A.S. Talsma,Ralph Müller,Maria Seton,Hans-Peter Bunge,Bernhard S. A. Schuberth,Grace E. Shephard,Christian Heine +7 more
TL;DR: In this article, the authors use geodynamic models with imposed plate velocities to test the forward-modeled history of subduction based on a particular plate motion model against alternative seismic tomography models.
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Absolute plate motions since 130 Ma constrained by subduction zone kinematics
TL;DR: In this article, a relative plate motion model is proposed for the last 130 Myr for a range of alternative reference frames, and quantitatively compare the results for times older than 70 Ma.
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Deformation-related volcanism in the Pacific Ocean linked to the Hawaiian–Emperor bend
John O'Connor,John O'Connor,Kaj Hoernle,R. Dietmar Müller,Jason Phipps Morgan,Nathaniel Butterworth,Folkmar Hauff,David T. Sandwell,Wilfried Jokat,Wilfried Jokat,Jan R. Wijbrans,Peter Stoffers +11 more
TL;DR: In this article, the authors analyzed the geochemical characteristics of lava samples collected from the Musicians Ridges, lines of volcanic seamounts formed close to the Hawaiian-Emperor bend, and found that the signature of these lavas is unlike typical ocean island basalts and instead resembles mid-ocean ridge basalts.
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Influence of overriding plate geometry and rheology on subduction
TL;DR: In this article, a Stokes flow solver based on the Boundary Element Method (BEM) with a Fast-Multipole (FM) implementation was used to study the evolution of the entire lithosphere-mantle system without imposing additional constraints in a whole-Earth spherical setting.