The terrestrial planets accreted from a diverse suite of solar system materials ranging from strongly O-deficient materials similar to enstatite chondrites via ordinary chondrite materials …
Seismic images of Earth's interior have revealed two continent-sized anomalies with low seismic velocities, known as the large low-velocity provinces (LLVPs), in the lowermost …
GyPSuM is a 3‐D model of mantle shear wave (S) speeds, compressional wave (P) speeds, and density. The model is developed through simultaneous inversion of seismic body wave …
Detailed global plate motion models that provide a continuous description of plate boundaries through time are an effective tool for exploring processes both at and below the …
We propose a new model of Earth's bulk composition based on enstatite chondrites (E- chondrites), the only chondrite group isotopically identical to the Earth. This model allows a …
TH Torsvik, R van der Voo… - Proceedings of the …, 2014 - National Acad Sciences
Earth's residual geoid is dominated by a degree-2 mode, with elevated regions above large low shear-wave velocity provinces on the core–mantle boundary beneath Africa and the …
Abstract The short-lived 182 Hf-182 W isotope system (t 1/2= 9 Ma) left evidence in both ancient and modern terrestrial rock record of processes that took place during the earliest …
V Lekic, S Cottaar, A Dziewonski… - Earth and Planetary …, 2012 - Elsevier
Earth's lower mantle is dominated by a pair of antipodal large low shear velocity provinces (LLSVPs) that reach> 1000km up from the core–mantle boundary (CMB). These are …
The composition of the lower mantle—comprising 56% of Earth's volume—remains poorly constrained. Among the major elements, Mg/Si ratios ranging from∼ 0.9–1.1, such as in …