This paper reviews different ways potential-field modelling systems represent the 3D
structure of the Earth's crust. 3D structures may be represented by discrete objects, voxels …

The kinematic evolution of the Pyrenees was largely controlled by structural and thermal
heterogeneities inherited from a precursor rift system, resulting in complex along-strike …

We study the age of the subducting Pacific slab beneath East Asia using a high-resolution
model of P-wave tomography and paleo-age data of ancient seafloor. Our results show that …

We have developed a geomechanically based restoration method to model reservoir
deformation. The approach, founded on the finite-element method, simulates the physical …

Recently, time and effort have been devoted to automatic texture mapping. It is possible to
study the parameterization function and to describe the texture mapping process in terms of …

Sedimentary basins host, among others, most of our energy and fresh-water resources: they
can be regarded as large geo-reactors in which many physical and chemical processes …

Balancing of structural cross sections is often hindered by a limited database or tectonic
complications. In such cases, kinematic constraints may help to better constrain the …

The inversion of multiple geoscientific datasets to define structures in hard rock terrains has
for the most part been limited to geophysical methods supported by rock property …

The “Bolivian orocline” is the change in trend of the Andes from NW to N near 18° S.
Paleomagnetic data have been used to infer that this bend was in part produced by …

In the era of big data and the rapid advancements in machine learning, particularly deep
learning, three-dimensional mineral prospectivity mapping (3D MPM) has emerged as a …