We present a review of the analogue modelling method, which has been used for 200 years,
and continues to be used, to investigate geological phenomena and geodynamic processes …

Earthquakes occur by overcoming fault friction; therefore, quantifying fault resistance is
central to earthquake physics. Values for both static and dynamic friction are required, and …

The study investigated geomorphology of the Japan Trench located east of Japan, Pacific
Ocean. A high-resolution GEBCO Gridded Bathymetric Dataset was used for modeling …

The mid-crustal ramp on the Main Himalayan Thrust (MHT) in the Lesser Himalaya
Sequence (LHS) is the most critical geometrical asperity to trigger major seismic events in …

The Pyrenees are a collisional orogen striking WNW-ESE. However, in the Ainsa oblique
zone in the south-central part of the Pyrenees, faults and folds rotate to∼ N–S over a …

Fold-and-thrust belts (FTBs) evolve over a mechanically weak basal décollement that
separates the overlying intensely deformed rocks from the underlying less deformed ones …

As an active margin of the Pacific Plate, the ocean‐continent transition zone records major
tectonic events from the Late Mesozoic to the present‐day. The development of the transition …

Fold and thrust belts (FTBs) accommodate tectonic convergence through folding and faulting
of crustal rocks during a collisional event between two continental plates. Although evidence …

This study integrates field evidence with laboratory experiments to show the mechanical
effects of a lithologically contrasting stratigraphic sequence on the development of frontal …

Deformation patterns caused by the subduction of a single seamount or aseismic ridge have
been well studied in analogue and numerical models. However, the effects of sequential …