Ocean Basin Evolution and Global-Scale Plate Reorganization Events Since Pangea Breakup
We present a revised global plate motion model with continuously closing plate boundaries ranging from the Triassic at 230 Ma to the present day, assess differences among alternative absolute plate…
Global plate boundary evolution and kinematics since the late Paleozoic
- K. Matthews, K. Maloney, S. Zahirovic, S. Williams, M. Seton, R. Müller
- Geology
- 1 November 2016
Tectonic evolution and deep mantle structure of the eastern Tethys since the latest Jurassic
- S. Zahirovic, K. Matthews, Michaell Gurnis
- Geology
- 1 November 2016
A Global Data Set of Present‐Day Oceanic Crustal Age and Seafloor Spreading Parameters
We present an updated oceanic crustal age grid and a set of complementary grids including spreading rate, asymmetry, direction, and obliquity. Our data set is based on a selected set of magnetic…
The tectonic fabric of the ocean basins
- K. Matthews, R. Müller, P. Wessel, J. Whittaker
- Geology
- 1 December 2011
[1] We present a global community data set of fracture zones (FZs), discordant zones, propagating ridges, V-shaped structures and extinct ridges, digitized from vertical gravity gradient (VGG) maps.…
Geologic and kinematic constraints on Late Cretaceous to mid Eocene plate boundaries in the southwest Pacific
- K. Matthews, S. Williams, J. Whittaker, R. Müller, M. Seton, G. Clarke
- Geology
- 1 April 2013
A global-scale plate reorganization event at 105−100 Ma
- K. Matthews, M. Seton, R. Müller
- Geology
- 15 November 2012
Global kinematics of tectonic plates and subduction zones since the late Paleozoic Era
- Alexander Young, N. Flament, R. Müller
- GeologyGeoscience Frontiers
- 1 May 2019
Formation of Australian continental margin highlands driven by plate-mantle interaction
- R. Müller, N. Flament, K. Matthews, S. Williams, M. Gurnis
- Geology
- 1 May 2016
On the consistency of seismically imaged lower mantle slabs
- G. Shephard, K. Matthews, Kasra Hosseini, M. Domeier
- GeologyScientific Reports
- 8 September 2017
To assess the robustness and distribution of positive seismic anomalies, inferred as subducted slabs, a set of vote maps for the lower mantle with 14 global P-wave or S-wave tomography models are created and the most consistent positive wavespeed features are identified by an increasing vote count.
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