Our understanding of folds and folding builds on detailed geometrical analysis. Proper
description of folds and their relation to other structures such as fractures, cleavage and …

Stretching of the Earth's upper crust is commonly accommodated by normal faulting, fault-
related folding and/or fracturing such as veins and joints. However, an increasing number of …

Abstract 3D seismic reflection imagery is the most widely used resource for interpreting the
geometric structure of faults in the subsurface. Yet these endeavours carry uncertainties, the …

Abstract The Rio do Peixe Basin is part of a series of aborted Cretaceous rifts formed within
the Proterozoic Borborema Province, onshore NE Brazil in response to rifting between Africa …

Fault-horizon cut-off data extracted from seismic reflection datasets are used to study normal
fault geometry, displacement distribution, and growth history. We assess the influence of …

The relationship between normal fault displacement (D) and length (L) varies due to
numerous factors, including fault size, maturity, basin tectonic history, and host rock …

Abstract The Porcupine Basin is a large underexplored sedimentary basin located offshore
west of Ireland within the structurally complex European North Atlantic Margin. The basin …

Many previous studies have shown that normal faults are formed by growth and linkage of
shorter fault segments through time and have suggested various fault growth models …

Abstract The NNW-SSE trending Sierra Palomera fault is characterized as an active, nearly
pure extensional fault with mean transport direction towards N230° E, consistent with the …