Publications associées à Discordance (stratigraphie)

To break or not to break: The role of secondary mineralisation on joint reactivation in sandstone

Alexandra Roma Larisa Kushnir, Michael Heap

Discontinuities, including fractures and joint sets, modify the fluid transport properties and strength of rock masses. While open fractures and joints increase rock mass permeability and decrease rock mass strength, fluid flow within these structures can ...

2023

Evolution of the hydromorphodynamics of mountain river confluences for varying discharge ratios and junction angles

Anton Schleiss, Mário Jorge Rodrigues Pereira Da Franca, Sebastián Guillén Ludeña, António Heleno Cardoso

Mountain river confluences are characterized by narrow and steep tributaries that supply abundant sediment load to a main channel that, in turn, provides the dominant flow discharge. In addition, bed sediments consist of poorly sorted mixtures that promote ...

Elsevier2016

Flow and sediment dynamics in bed discordant channel confluences

Anton Schleiss, Koen Blanckaert, Marcelo Leite Ribeiro

Confluences between small steep tributaries with dominant supply of poorly sorted sediment and larger main channels with dominant flow supply, which are characterized by a pronounced bed discordance, have not yet been considered in the literature. The hydr ...

Tsinghua University Press2011

A study of the dynamics of saturated granular assemblages and its implications for transport, stress propagation and failure in marine sediments

Nicolas Le Dantec

The subject of small-scale marine sediment mechanics is an area of active research, motivated by its key role in beach and shelf processes. Much of the existing small-scale work has focused on two-phase flows and particle behavior at the sediment interface ...

University of California San Diego2009

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Discordance (stratigraphie)

To break or not to break: The role of secondary mineralisation on joint reactivation in sandstone

Evolution of the hydromorphodynamics of mountain river confluences for varying discharge ratios and junction angles

Flow and sediment dynamics in bed discordant channel confluences

A study of the dynamics of saturated granular assemblages and its implications for transport, stress propagation and failure in marine sediments

Immobilization of uranium in contaminated sediments by hydroxyapatite addition

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Chattez avec Graph Search

Immobilization of uranium in contaminated sediments by hydroxyapatite addition

Flow and sediment dynamics in bed discordant channel confluences

Evolution of the hydromorphodynamics of mountain river confluences for varying discharge ratios and junction angles

To break or not to break: The role of secondary mineralisation on joint reactivation in sandstone

A study of the dynamics of saturated granular assemblages and its implications for transport, stress propagation and failure in marine sediments