Accurate spatial models of tectonic plates and geological terranes are important for
analyzing and interpreting a wide variety of geoscientific data and developing compositional …

We focus on the southern North Atlantic rifted margins to investigate the partitioning and
propagation of deformation in hyperextended rift systems using plate kinematic modeling …

The second generation Antarctic magnetic anomaly compilation for the region south of 60° S
includes some 3.5 million line‐km of aeromagnetic and marine magnetic data that more than …

Our understanding of continent-ocean transition structures and magmatism in the absence
of excessive magmatic additions has been guided by the observations and models …

The computer-based modeling of geological and geophysical data allows the construction of
3D geological models that can predict the location of differing lithologies, intrusive units and …

Three crustal-scale sequentially restored cross-sections along the Central External Betic
Cordillera enable us to pinpoint the role of extreme crustal thinning, tectonic inheritance and …

The nature and origin of the J‐magnetic anomaly along the Iberia–Newfoundland margins
are controversial and its validity for plate kinematic reconstructions questioned. At present, it …

Despite post-processing efforts by space agencies and research institutions, contemporary
global digital elevation models (DEMs) may contain artefacts, ie, erroneous features that do …

It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …

We present a refined map of geothermal heat flow for Antarctica, Aq1, based on multiple
observables. The map is generated using a similarity detection approach by attributing …