Salles, Tristan; Flament, Nicolas; Muller, R. Dietmar
Recent studies of the past eastern Australian landscape from present-day longitudinal river profiles and from mantle flow models suggest that the interaction of plate motion with mantle convection accounts for the two ...
Hassan, Rakib; Gurnis, Michael; Williams, Simon E.; Muller, R. Dietmar
Numerical models of landscape evolution are playing an increasingly important role in providing an improved understanding of geomorphic transport processes shaping Earth's surface topography. Improving theoretical underpinnings ...
Cao, Wenchao; Zahirovic, Sabin; Flament, Nicolas; Williams, Simon E; Golonka, Jan; Muller, R. Dietmar
Paleogeographic reconstructions are important to understand Earth's tectonic evolution, past eustatic and regional sea level change, paleoclimate and ocean circulation, deep Earth resources and to constrain and interpret ...
Brune, Sascha; Williams, Simon E; Muller, R. Dietmar
Movements of tectonic plates often induce oblique deformation at divergent plate boundaries. This is in striking contrast with traditional conceptual models of rifting and rifted margin formation, which often assume 2-D ...
Gurnis, Michael; Yang, Ting; Cannon, John S; Turner, Mark; Williams, Simon E; Flament, Nicolas; Muller, R. Dietmar
Traditional plate reconstruction methodologies do not allow for plate deformation to be considered. Here we present software to construct and visualize global tectonic reconstructions with deforming plates within the context ...
Matthews, Kara J; Muller, R. Dietmar; Sandwell, David T
Mapping of seafloor tectonic fabric in the Indian Ocean, using high-resolution satellite-derived vertical gravity gradient data, reveals an extinct Pacific-style oceanic microplate ('Mammerickx Microplate') west of the ...
Muller, R. Dietmar; Flament, Nicolas; Matthews, Kara J; Williams, Simon E; Gurnis, Michael
Passive margin highlands occur on most continents on Earth and play a critical role in the cycle of weathering, erosion, and atmospheric circulation. Yet, in contrast to the well-developed understanding of collisional ...
Cao, Xianzhi; Flament, Nicolas; Muller, R. Dietmar; Li, Shanzhong
Some changes in the topography of eastern China since Late Jurassic times cannot be well explained by lithospheric deformation. Here we analyze global mantle flow models to investigate how mantle-driven long-wavelength ...
Rubey, Michael; Brune, Sascha; Heine, Christian J; Davies, Rhodri D; Williams, Simon E; Muller, R. Dietmar
We evaluate the spatial and temporal evolution of Earth's long-wavelength surface dynamic topography since the Jurassic using a series of high-resolution global mantle convection models. These models are Earth-like in terms ...
Atmospheric carbon dioxide (CO2) data for the last 420 million years (My) show long-term fluctuations related to supercontinent cycles as well as shorter cycles at 26 to 32 My whose origin is unknown. Periodicities of 26 ...
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