Results 71 to 80 of about 5,770 (227)
A three dimensional (3D) finite element model is used to study the conditions leading to mechanical decoupling at a salt layer and vertically varying stress fields in salt-bearing sedimentary basins.
Steffen Ahlers +2 more
doaj +1 more source
Troodos: A Giant Serpentinite Diapir
Troodos is a classical ophiolite complex. It is proposed that the serpentinized harzburgites that now form the top of the mountain and represent the originally lowest part of the ophiolite sequence rose as a diapir. This diapiric rise is caused by the pervasive serpentinization of a suboceanic harzburgite, due to rock-sea water interaction.
openaire +3 more sources
Coronae on Venus observations and models of origin [PDF]
The Venera 15/16 spacecraft revealed a number of features of unknown origin including coronae, elongate to circular structures with a complex interior surrounded by an annulus of concentric ridges. Eighteen coronae were identified in Venera 15/16 data of
Stofan, E. R.
core +1 more source
Modelización Gravimétrica 3D del diapiro de Cardona, Cuenca del Ebro (NE de España) [PDF]
En este trabajo se presentan los resultados derivados de la interpretación de 320 estaciones gravimétricas realizadas sobre el diapiro de Cardona con el objetivo de obtener información sobre su geometría tridimensional.
Casas i Ponsatí, Albert +3 more
core
Abstract At the northern Hikurangi margin, Aotearoa New Zealand, slow slip events (SSEs) recur every 6–24 months to ∼ ${\sim} $30 km depth. Although shallow SSEs (0–10 km) are well‐studied offshore, the deeper portion (10–30 km) remains poorly understood, limiting insight into SSE initiation.
Amy Woodward +11 more
wiley +1 more source
The role of nonuniform internal heating in Triton's energy budget [PDF]
Triton's large heliocentric distance and high albedo, combined with its unusually large silicate mass fraction, make internal heating more important in its energy budget than in that of any other icy satellite. Brown et al.
Brown, R. H., Kirk, R. L.
core +1 more source
Mechanisms and Geochemical Models of Core Formation
The formation of the Earth's core is a consequence of planetary accretion and processes in the Earth's interior. The mechanical process of planetary differentiation is likely to occur in large, if not global, magma oceans created by the collisions of ...
Abe +74 more
core +1 more source
Surface subsidence above salt mines reflects the complex interaction of elastic and viscous deformation processes in rock salt, as well as hydrogeological and structural changes within diapiric formations.
Maj Agnieszka
doaj +1 more source
The Mesozoic subduction zone over the Dongsha Waters (DSWs) of the South China Sea (SCS) is a part of the westward subduction of the ancient Pacific plate.
Pibo Su, Zhongquan Zhao, Kangshou Zhang
doaj +1 more source
The effect of sunlight on the surface of Triton was studied. Widely disparate models of the active geysers observed during Voyager 2 flyby were proposed, with a solar energy source almost their only feature.
Brown, R. H., Kirk, R. L.
core +1 more source

