Results 171 to 180 of about 59,876 (275)
Abstract The Late Cretaceous Oman ophiolite includes a series of volcanic rocks generated during the transition from spreading ridge to protoarc associated with subduction initiation. We analyzed major and trace elements and Sr, Nd, and Pb isotope compositions of lavas and dikes of the protoarc stage, especially boninites. We also analyzed amphibolites
Tsuyoshi Ishikawa +6 more
wiley +1 more source
The glass-ceiling convective regime and the origin and diversity of coronae on Venus. [PDF]
Kerr MC +3 more
europepmc +1 more source
Mantle Transition Zone Topography in New Zealand From Teleseismic P $P$‐Wave Receiver Functions
Abstract The geology of New Zealand has been shaped by tectonic plate interactions driven by mantle convection over the past 60 million years, but the effects of these interactions on the transition to the lower mantle are not yet well understood. We analyze 10 years of teleseismic P $P$‐wave receiver functions using common conversion point stacking to
Quan Zhang +4 more
wiley +1 more source
The importance of past rifting in large igneous province development. [PDF]
Kounoudis R +7 more
europepmc +1 more source
Numerical Modeling of Purely Active (Plume‐Produced) Continental Rifting and Break‐Up
Abstract In contrast to the traditional mechanism of passive continental rifting (driven by far‐field tectonic forces), the active rifting‐to‐break‐up processes (caused by rising mantle plumes) are still poorly understood. However, most episodes of fragmentation of the last supercontinent Pangea were relatively shortly preceded (within ∼10 Myr) by the ...
Alexander Koptev +12 more
wiley +1 more source
Abstract Silicate melts play a crucial role in planetary differentiation. The density contrast between silicate melts and the surrounding solid residue exerts a primary control on many magmatic processes. However, direct measurements of the density of silicate melts at high pressure (P) and temperature (T) conditions remain challenging, particularly ...
Man Xu +6 more
wiley +1 more source
The sub-arc mantle has remained oxidized since the Neoproterozoic oxygenation event. [PDF]
Liu CT, Ye CY, Xia QK, ZhangZhou J.
europepmc +1 more source
Origin of the Bulge Topography Within Caloris Basin, Mercury
Abstract Caloris basin on Mercury has a massive circular bulge topography imprinted with unique fault sets. A variety of deformational processes have been proposed to have influenced their formation, including both global contraction and basin evolution, as well as the deposition and weight of the volcanic infill.
G. Schmidt +6 more
wiley +1 more source
Dissecting the puzzle of tectonic lid regimes in terrestrial planets. [PDF]
Lyu T +6 more
europepmc +1 more source

