• Oceanic microplate formation records the onset of India-Eurasia collision 

      Matthews, Kara J; Muller, R. Dietmar; Sandwell, David T
      Published 2016-01-01
      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 ...
      Open Access
      Article
    • Global patterns in Earth's dynamic topography since the Jurassic: The role of subducted slabs 

      Rubey, Michael; Brune, Sascha; Heine, Christian J; Davies, Rhodri D; Williams, Simon E; Muller, R. Dietmar
      Published 2017-09-11
      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 ...
      Open Access
      Article
    • Improving global paleogeography since the late Paleozoic using paleobiology 

      Cao, Wenchao; Zahirovic, Sabin; Flament, Nicolas; Williams, Simon E; Golonka, Jan; Muller, R. Dietmar
      Published 2017-12-04
      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 ...
      Open Access
      Article
    • Oceanic crustal carbon cycle drives 26-million-year atmospheric carbon dioxide periodicities 

      Muller, R. Dietmar; Dutkiewicz, Adriana
      Published 2018-02-02
      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 ...
      Open Access
      Article
    • Oblique rifting: The rule, not the exception 

      Brune, Sascha; Williams, Simon E; Muller, R. Dietmar
      Published 2018-10-26
      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 ...
      Open Access
      Article