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10.1007/S00193-021-00999-8

## High-energy non-equilibrium flows of air and $$\hbox {CO}_2$$ – $$\hbox {N}_2$$ over a double-wedge geometry are studied numerically.

Shock interactions in inviscid air and $$\hbox {CO}_2$$–$$\hbox {N}_2$$ flows in thermochemical non-equilibrium

10.1038/s41561-021-00779-0

## We find that the pattern of background seismicity correlates with the margin-parallel long-wavelength wedge geometry and with published estimates of geologic-timescale coastal uplift.

Contribution of background seismicity to forearc uplift

## The length scale $d_{s}$ is related to the work performed by TRC mixing using an idealized well-mixed wedge geometry.

The self-similar stratified inner-shelf response to transient rip-current-induced mixing

## This offers a new perspective on the role of sediments, suggesting that sediment buoyancy and wedge geometry also play an important role on large-scale subduction dynamics.

The role of sediment subduction and buoyancy on subduction dynamics and geometry

10.1016/J.TECTO.2019.04.026

## Its crustal geometry consists of a thrust wedge geometry of the European lithosphere between the Axial Zone imbricate system of the Iberian upper crust and the north-directed subduction of the Iberian lower crust.

Crustal-scale balanced cross-section and restorations of the Central Pyrenean belt (Nestes-Cinca transect): Highlighting the structural control of Variscan belt and Permian-Mesozoic rift systems on mountain building

10.1007/s12303-019-0023-x

## Assuming that the cohesion is very low, we could infer the ranges of strengths that most observed wedge geometry data have 0.

Numerical simulation of hydro-mechanical constraints on the geometry of a critically tapered accretionary wedge

10.1016/J.JSG.2018.12.002

## Application of the analytical and homogeneous critical Coulomb wedge (CCW) theory to the MFTB closely predicts the external wedge geometry but fails to predict the observed shortening of the individual litho-tectonic units and structural styles.

Quantifying frictional variations and erosion in the Mexican fold-thrust belt

## A simple two-dimensional wedge geometry was selected to simulate the flow structure found in atmospheric reentry.

Spectroscopy of high speed expanding argon flows

10.1016/J.AST.2019.07.013

## 1 MJ/kg stagnation enthalpy, and Mach 7 nitrogen and air flows at 8 MJ/kg stagnation enthalpy over a double wedge geometry have been reproduced numerically assuming chemical and thermal non-equilibrium.

Computational investigations into heat transfer over a double wedge in hypersonic flows

10.1016/J.MECHMAT.2019.103088

## Cleavage through the insertion of a rounded wedge provides a straightforward mechanical setup that produces stable crack propagation, so long as the effects of friction and wedge geometry are properly considered.

Obreimoff revisited: Controlled heterogeneous fracture through the splitting of mica

10.1016/J.EPSL.2019.02.011

## Wedge geometry – associated with discordant contacts between different lithologies – causes constructive and destructive amplitude interference, creating imaging artefacts of sandstone thickness and geometry.

Seismic imaging of complex geometry: Forward modeling of sandstone intrusions

Wedge Geometry
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