Patrick Launeau

Fabric characteristics of subaerial slope deposits

Tectonic map and overall architecture of the Alpine orogen

The Cuaró Mesozoic doleritic dyke swarm, southern Paraná basin, Uruguay: Examples of superimposed magnetic fabrics?

Classification of trabeculae into three‐dimensional rodlike and platelike structures via local inertial anisotropy

BoneJ: Free and extensible bone image analysis in ImageJ

Granite magma formation, transport and emplacement in the Earth's crust

Graphical representation of particle shape using triangular diagrams: an Excel spreadsheet method

Melting of the continental crust during orogenesis: the thermal, rheological, and compositional consequences of melt transport from lower to upper continental crustThis article is one of a selection of papers published in this Special Issue on the the themeLithoprobe—parameters, processes, and the evolution of a continent.

On ultrahigh temperature crustal metamorphism: Phase equilibria, trace element thermometry, bulk composition, heat sources, timescales and tectonic settings

Symmagmatic folding of the base of the Bergell pluton, Central Alps

An overview of adakite, tonalite–trondhjemite–granodiorite (TTG), and sanukitoid: relationships and some implications for crustal evolution

Syntectonic granite emplacement at different structural levels: the Closepet granite, South India

The new global lithological map database GLiM: A representation of rock properties at the Earth surface

The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot Zones

Fabric analysis using the intercept method

Magnetic fabric evidence for conduit‐fed emplacement of a tabular intrusion: Dinkey Creek Pluton, central Sierra Nevada batholith, California

Fabric of the Rio Ceará–Mirim mafic dike swarm (northeastern Brazil) determined by anisotropy of magnetic susceptibility and image analysis

Magmatic fabric acquisition mechanisms in a syenite: Results of a combined anisotropy of magnetic susceptibility and image analysis study

Evidence of magmatic flow by 2-D image analysis of 3-D shape preferred orientation distributions

Mechanisms and duration of non-tectonically assisted magma emplacement in the upper crust: The Black Mesa pluton, Henry Mountains, Utah

Effect of mechanical interactions on the development of shape preferred orientations: a two-dimensional experimental approach